10 February 2015, Volume 26 Issue 2
    

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  • ZHANG Kang,LI Tie-jun
    Natural Gas Geoscience. 2015, 26(2): 199-207. https://doi.org/10.11764/j.issn.1672-1926.2015.02.0199
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          Long-standing and increasing undeveloped natural gas reserve is one of the characteristics in exploration and production of natural gas in China.Analysis on its development process and its distribution in different basins is a necessary precondition for increasing reserve producing rate and keeping enhancement of production.Undeveloped geological reserve of natural gas in China in 2013 was about 5.62 trillion cubic meters with its undeveloped rate of 42.3%,while undeveloped recoverable reserve is 0.535 4 trillion cubic meters with its undeveloped rate of 23.7%.According to the analysis of the distribution of basins and companies of undeveloped reserves and different oilfields,some issues are raised under the condition of new ideas and technologies:(1) undeveloped reserves are the realistic regions for enhancement|(2) insight into present situation and dynamic state of proved reserves|(3) the key is the application of proper technologies.Issues,including specialty of each undeveloped reserve,new round deliberate seismic work,moderate lead-in of drilling and reservoir reconstruction,advanced methods in developing middle-small gas fields and more attention on development of dissolved gas,should be emphasized.Three national oil companies should concentrate on making contribution to natural gas production enhancement,narrowing block area,enhancing recovery so as to achieve return on capital and economic benefits.

  • SHI Shu-yuan,HU Su-yun,LIU Wei,XU Zhao-hui,LI Bo-hua,WU Na
    Natural Gas Geoscience. 2015, 26(2): 208-217. https://doi.org/10.11764/j.issn.1672-1926.2015.02.0208
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    Paleokarst reservoir is an important target for hydrocarbon exploration and development.Distinguishing of paleokarst development period is always a difficulty facing modeling of paleokarst reservoir.The existing methods for identifying paleokarst period are mostly based on exposure features.
    But paleokarstification involves various forms,with some lacking of exposure features,such as hydrothermal flow paleokarstification.Thus,we put forward a comprehensive method involving carbon and oxygen isotopic characteristics of paleokarstic fillings and fluid inclusions characteristics.Based on abundant outcrop data of Tarim Basin,we then analyze the multiple inclusions,and get an average uniform temperature distribution chart based on division of diagenesis sequence.Contrasting discriminant chart of carbon and oxygen isotopes and inclusions homogenization temperature diagram can be used for judging the paleokarst development time.The δ13C-δ18O crossplot,according to the combination of core and cutting relation,was divided into different filling period time chart that are included in the distribution range of values.We apply these charts in period distinguishing of Ordovician paleokarst in Halahatang area and get a well matched result with those obtained based on regional geological background and seismic data interpretation.

  • LI Meng,TANG Liang-jie,QI Li-xin,HUANG Tai-zhu,ZHEN Su-jing,TIAN Ya-jie
    Natural Gas Geoscience. 2015, 26(2): 218-228. https://doi.org/10.11764/j.issn.1672-1926.2015.02.0218
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    The evolution of the south slope of Tabei Uplift was characterized by multiple epochs and horizontal differentiation,which determines vertically and laterally imbalances of hydrocarbon distribution.Based on an integrated analysis,temporal and spatial variation of sub-structural units and geological conditions as hydrocarbon source rocks and reservoir-cap assemblages,this paper discussed the controlling factors of differential evolution on hydrocarbon accumulation of three petroleum bearing groups in the South Slope of Tabei Uplift.For the Lower-Paleozoic carbonates petroleum-bearing group,tectonic location and concave-convex structure determine oil source and migration direction respectively,and diversity of reservoir-cap assemblages is related to multi-stage of uplifting,erosion and karstification.Akekule,Yingmaili and Halahatang have superior hydrocarbon accumulation condition and great geological configuration.For the Paleozoic petroleum-bearing clastic rock group,diverse uplift and denudation limit the distribution and thickness of favorable reservoir,and also affect their reservoir performance.Trap characteristics determine the size of the oil and gas infilling,for anticlinal trap of Donghetang Oilfield have experienced two oil and gas charging stages.Oil source and migration conditions such as fault and sand are the major factors which influence lateral imbalance of the Mesozoic-Cenozoic petroleum-bearing clastic rock group.Oil and gas of Akekule and Halahatang mainly come from the underlying Palaeozoic marine oil-bearing series,with a high migration efficiency of source rock-rooted faults and sandbody.
     
  • GENG Xiao-jie,LIN Chang-song,HAN Jian-fa,YIN Hong,LI Hao,YANG Zhao-shuan,WANG Qing-long
    Natural Gas Geoscience. 2015, 26(2): 229-240. https://doi.org/10.11764/j.issn.1672-1926.2015.02.0229
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    FMI (Formation Micro-Scanner Image) is widely used to analyze reservoir properties with the advantages of high resolution,visible and quantified.In this study,11 FMI facies are classified based on the combination of borehole images,cores,thin sections and open-hole logs.It includes reservoir types like carves and tectonic fractures,sedimentary interlayer types like high resistivity facies and two compound facies of fractures and holes.Besides description of karst systems in borehole images,anomalies in GR curve attracting the researchers are analyzed by FMI images.It shows that compound facies of fractures and holes could be effective reservoir instead of caves with high GR value because oil/gas-bearing holes are connected by fractures.Two suites of karst system were formed in the OY1 while small scale caves and holes were formed in the OY2 because of lithological and structure locations.The results of this study demonstrated that,uncomformity and tectonic geomorphology control the differences of the paleokarst system.

  • REN Ping,LIN Chang-son,HAN Jian-fa,LI Hao,LIU Jing-yan,WANG Qing-long
    Natural Gas Geoscience. 2015, 26(2): 241-251. https://doi.org/10.11764/j.issn.1672-1926.2015.02.0241
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    The depositional microfacies of carbonate illustrate the feature of the depositional water energy and environment.Additionally,microfacies are the fundamental of pore space development and facilitate the formation of favorable reservoirs.Ten depositional microfacies (Mf1-Mf10) and four microfacies patterns (MA1-MA4) are recognized in Yingshan Formation,the northern slope of central Tarim Basin,through a large number of thin-sections and cores.The microfacies patterns are distributed horizontally along with the Tazhong No.1 fault zone.High-energy to medium-to-high-energy depositional patterns developed beside the boundary of platform (i.e.MA1 and MA2).However,the microfacies patterns in the inner platform indicate the decrease of water-energy to the central basin.Two microfacies patterns,including medium-to-low-energy tidal flat (MA3) and low-energy-dolomitic tidal flat (MA4),have been suggested in the inner platform.Medium-to-low-energy microfacies patterns transform to medium-to-high-energy microfacies patterns from Yingshan 2nd to Yingshan 1st.During the late stage of Yingshan 1st,which is the main stage for forming carbonate shoals,the depositional water energy gradually increased from the bottom to the top.The high energy microfacies which were on the top of Yingshan Formation,were the primitive material for favorable reservoir,because they formed several types of pores,and developed structural fractures and karstification more easily.
  • MENG Qing-yang,GUI Li-li,CHEN Yan,YUAN Li,YANG Fan,SUI Li-wei,BAI Dong-lai
    Natural Gas Geoscience. 2015, 26(2): 252-260. https://doi.org/10.11764/j.issn.1672-1926.2015.02.0252
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    The hydrocarbon charging history of Hongliuquan oilfield,Gasikule oilfield and Yingdong oilfield is studied in this paper by synthetically adopting fluid inclusion petrography,fluorescence spectrum,infrared spectrum,microthermometry analysis and burial history modelling.The results illustrate that grain with oil inclusions is well developed in the southwestern Qaidam Basin with the index of grain with oil inclusion (GOI) value between 5%-90%.According to the characteristics of fluorescence color,occurrence,host mineral of oil inclusion,two fluid inclusion assemblages can be classified as yellow fluorescence inclusion and blue fluorescence inclusion.The peak of fluorescence spectrum and methyl content of infrared spectrum both reflect that the maturity of blue fluorescence inclusion is higher than that of yellow fluorescence inclusion.Combined with homogenization temperature of fluid inclusions and thermal evolution analysis,it is confirmed that there were mainly two episodes of hydrocarbon charging in the southwestern Qaidam Baisn.The charging time of Gasikule oilfield and Hongliuquan oilfield is 26Ma and 10Ma,respectively.The charging time of Yingdong oilfield is separately 10Ma and 5Ma.The later hydrocarbon charging process and tectonic evolution control the preservation condition and hydrocarbon enrichment.

  • LIU Jin-hua,WU Li-feng,WU Yan-mei,LIU Jian,LUO Hong-fei
    Natural Gas Geoscience. 2015, 26(2): 261-268. https://doi.org/10.11764/j.issn.1672-1926.2015.02.0261
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    Fan-delta was developed in the Dainan Formation of Gaoyou Sag,and the distribution of the sandbody was controlled by the distributary channel,but the existence of many lenticular oil-sand is inconsistent with the distribution of reservoir,so we do the genetic research on the lenticular sand.The overlapping oil-bearing area of Dainan Formation is continuous,but the oil-bearing area of the single sublayer is lenticular or allantoid.By the analysis of the water injection response,the communication of the sand is bad,response wells are little,the better response wells followed the provenance direction,but the distance of the response well is short,so the characteristic of the water injection showed that the reservoirs of the work area are with higher anisotropy.After the observation of well core,there are many soft sediment deformations,and on the base of the foreign experience,especially the theory of detrital liquid by Shanmugam,the small-size olistostrome genetic model of lithologic hydrocarbon reservoir was set up,and we think that the lenticular oil-sand was formed by the olistostrome in the layer,and the soft sediment deformation caused the bad physical property of the reservoir,so the distribution of the oil sand became lenticular.
  • LI Ji-yan,SONG Guo-qi,WANG Xiao-lei,CHEN Jing-jing,SONG Ming-fu
    Natural Gas Geoscience. 2015, 26(2): 269-276. https://doi.org/10.11764/j.issn.1672-1926.2015.02.0269
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    To analyze the controlling influence of original sedimentary environment on diagenesis,and highlight the distinctiveness of the diagenesis of the red-bed reservoir,based on various analyses such as thin section identification,scanning electron microscope,core analysis,X-ray diffraction mineral analysis,etc.,alluvial plain of Wangjiagang and beach-bar of Boxing were selected for a comparative research between red-bed sandstone and grey-bed sandstone.The paper qualitatively analyzed the diagenetic characteristics and quantitatively calculated the diagenetic products,evolution process of diagenetic porosity with two types of sandbody.The results show that,grey-bed beach sandstones have characteristics of late ferrous-bearing carbonate cements,strong compaction,strong denudation|Red-bed reservoirs have characteristics of early carbonate cementation,weak compaction,and weak denudation.The two kinds of sandbodies experienced diagenesis of different intensity,resulting in the obvious difference between the diagenetic porosity evolution and pore types of reservoir,red-bed reservoir is mainly primary pore,reservoir of beach-bar sandstone is dominated by secondary pores.

  • ZHENG Min,JIA Cheng-zao,WANG Wen-guang,LI Peng,LI Jian-zhong,WU Xiao-zhi,ZHANG Yong-feng
    Natural Gas Geoscience. 2015, 26(2): 277-291. https://doi.org/10.11764/j.issn.1672-1926.2015.02.0277
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    The marine superimposed basins are rich in oil-cracking gas resources.Their hydrocarbon accumulation processes of late stage have experienced early paleo-oil reservoir accumulation period and late oil-cracking gas period,which are apparently controlled by tectonic evolution.Studying the relationship between tectonic evolution and oil-cracking gas accumulation of late stage has great significance to guide the exploration of oil-cracking gas reservoirs.Taking the relationship between tectonic evolution and oil-cracking gas accumulation of late stage for the Shunan area in the Sichuan Basin as an example,through the analysis on the responds of structural evolution to deposition,the relationship between hydrocarbon generation process of ancient source rocks,initial hydrocarbon accumulation,oil cracking and gas accumulation of late stage was studied.The source rocks of the Cambrian Qiongzhusi Formation in the Shunan area experienced three periods of hydrocarbon generation and two lag periods of hydrocarbon generation.During the large-scale tectonic uplift and thick erosion event in the periods of the Caledonian and the Hercynian,source rocks of the Qiongzhusi Formation had experienced two periods of hydrocarbon generation and two lag periods of hydrocarbon generation.The overlying super-thick strata deposited during the Indosinian and Yanshan periods made the source rocks of the Qiongzhusi Formation continuously generate oil and gas.The crude oil in the paleo-reservoir of the Longwangmiao Formation experienced one time of oil-cracking gas process.After the Indo-Chinese Epoch,the burial depth of the Triassic was deep enough to promote the crude oil in the paleo-reservoir of the Longwangmiao Formation to crack into gas.This process continued to the Late Yanshan Period,providing sufficient gas source.The following five conclusions are obtained:(1)The tectonic and depositional evolution of the marine superimposed basins controlled the development of the basic hydrocarbon geological conditions|(2)The tectonic and depositional evolution controlled the hydrocarbon generation process of the ancient source rocks;(3)The tectonic and depositional evolution controlled the development of the paleo-structures,accumulation and preservation of the paleo-oil reservoirs;(4)The tectonic and depositional evolution controlled the crude oil cracking of paleo-reservoirs and their accumulation in the late stage|(5)The research idea on oil-cracking gas accumulation of late stage of ancient marine source rocks was established,which could provide references for the paleo-oil reservoirs of the same type in order to expand the exploration scopes of oil-cracking gas reservoirs.
  • SU Ao,CHEN Hong-han,MA Yu-hua,ZHAN Hai-yong,YANG Wen-shuai
    Natural Gas Geoscience. 2015, 26(2): 292-300. https://doi.org/10.11764/j.issn.1672-1926.2015.02.0292
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    There was extensive evaporative fractionation effect in Xihu Depression,Eastern Sea Basin.However,most of the previous study on the gas washing is qualitative description.Taking Kongqueting region in Pinghu structural belt as an example,based on the geochemical characteristics and fracture characteristic,this paper discussed geologic conditions and main controlling factors of gas washing and analyzed effect of hydrocarbon reservoir by fluid inclusion system analysis technology and n-alkanes testing method.These findings suggest that coal measures which can generate gas continuously have abundant organic matter and provide good source rocks.Numerous faults and good match between oil and gas filling time result in the occurrence of gas washing in the Kongqueting region.Quantitative calculation of gas washing fractionation effect show that n-alkane loss rate of crude oil in the wells in the study area is 35.3% to 97.1% and break number is 18 to 27.Source distance and vertical depth control strength of gas washing fractionation effect.Besides,the former is more powerful controlling function than the latter.Gas washing fractionation effect not only makes gas layers and ratio of condensate gas layers decrease along the direction of the gas invasion,but also leads to the pattern of oil reservoir above gas reservoir and formation of condensate with low wax content and condensate gas with high wax content.

  • ZHOU Qing-hua,SONG Ning,WANG Cheng-zhang,LI Bo,CHE Jian-wei,PENG Chuan-sheng,XU Jiang-qiao
    Natural Gas Geoscience. 2015, 26(2): 301-311. https://doi.org/10.11764/j.issn.1672-1926.2015.02.0301
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    The Lower Cambrian Niutitang Formation in Changde region of Hunan Province is regarded as an important shale gas exploration layer.The Niutitang Formation is mainly composed of carbon-enriched siliceous shale,carbonaceous shale and stone coal.Based on the observation of field outcrops,well cores and regional geology data,integrating with analysis of rock organic geochemistry,mineral content,reservoir space type,physical mechanical properties and gas content,the features of shale in Niutitang Formation are studied in detail.The results indicate that shale in the Niutitang Formation is characterized by stable thickness and wide distribution areas,high organic carbon content,high levels of thermal evolution,large specific surface area with micro pore and fracture,and good gas adsorption ability.The mineral composition is dominantly clastic quartz and clay minerals,with feldspar,calcite,dolomite,pyrite and so on.The shale reservoir with high brittle mineral is easy to fracture.The shale real thickness of CY1 well is more than 310m,and the gas content is 0.5-2.1m3/t.It shows good reservoir conditions.The comprehensive evaluations by this paper indicate that this area has good shale gas exploration prospect.
     
  • LIN Tuo,ZHANG Jin-chuan,BAO Shu-jing,YANG Sheng-yu,LI Bo,HE Wei
    Natural Gas Geoscience. 2015, 26(2): 312-319. https://doi.org/10.11764/j.issn.1672-1926.2015.02.0312
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    Based on field geological investigation,combined with structural and sedimentary setting,well Changye 1 which is the first investigation well aimed to the Niutitang Formation shale gas in Hunan was selected and drilled with priority.By sampling,experimental analysis,well site desorption test,the gas content characteristic of the Niutitang Formation marine shale was quantitatively analyzed.The results show that Changde City peripheral and Cili-Shimen-Lixian areas are favorable region for optimum selection of investigation well of shale gas.Well Changye 1 reveals 674.5m of the Niutitang Formation organic-rich shale,which is the biggest thickness of black shale in China up to now.Its TOC, gas content from well site desorption,gas content from isothermal adsorption simulation test have a clear positive correlation,with the features of increasing from top to the middle-lower,then decreasing to the bottom.The black shale in 1 067-1 250m which is also the middle-lower part of the Niutitang Formation is the most valuable depth of well Changye 1,which have a good exploration prospect,with 10.14% of average TOC,3.7-5.8 m3/t of gas content from isothermal adsorption simulation test,0.5-2.1 m3/t of gas content from well site desorption.
  • ZHANG Shun,CHEN Shi-yue,YAN Ji-hua,TAN Ming-you,ZHANG Yun-yin,GONG Wen-lei,WANG Guang-zeng
    Natural Gas Geoscience. 2015, 26(2): 320-332. https://doi.org/10.11764/j.issn.1672-1926.2015.02.0320
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    Shale lithofacies is the main factor leading to the change of its physical properties and internal oil-gas distribution.Though usually seemed simple,fine-grained deposits actually contain complex rock types.This paper,using detailed description of core,thin sections identification,analysis of whole rock X-ray diffraction and scanning electron microscopy technologies,based on integrating various factors,such as mineral composition,sedimentary structure,organic matter abundance,color and other foreign matters,sets up a lithofacies classification scheme that is suitable for the shale in the 3rd and 4th members of Shahejie Formation in the west part of Dongying area.The most developed five types of lithofacies include organic-rich laminated limestone,organic-rich calcareous inter-bedded limestone,organic-contained fine-grained mixed sedimentary rocks,organic-lean massive clay stone and organic-rich laminated clay stone.And in those fine-grained deposits,the following reservoir space types are mainly developed,including structural,abnormal pressure and inter-laminar fracture,dissolution and inter-granular pores of clay mineral and inter-granular pores of calcite layer etc.Based on the above lithofacies and reservoir space analysis,the intercalation of limestone,laminated limestone and clay stone were identified as advantaged lithofacies in this area,which forms the basis of the exploration of the shale in this area.
  • MENG Qiang,WANG Xiao-feng,WANG Xiang-zeng,ZHANG Li-xia,JIANG Cheng-fu,LI Xiao-fu,SHI Bao-guang
    Natural Gas Geoscience. 2015, 26(2): 333-340. https://doi.org/10.11764/j.issn.1672-1926.2015.02.0333
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    Taking the Yishan slope southeast Chang7 shale of Yanchang Formation in the Ordos Basin as an example,with  desorption experiments of more than 30 shale samples,this paper studied the variation of carbon isotopic composition of alkanes during the shale gas desorption process,also discussed the possible causes of this phenomenon and its geological significance.The study found that carbon isotopic composition become higher by 9.2‰ ( from -50.1‰ to -40.9‰) for methane of desorbed gas (δ13C1),become higher by 2.8‰ ( from -35.5‰ to -32.7‰) for ethane (δ13C2 ),and nearly no change for propane during the desorption process.At room temperature or constant temperature,carbon isotopic composition of methane and ethane (δ13C1 & δ13C2) continuously increases.When the temperature rises,δ13C1 & & δ13C2 values suddenly become low first and then slowly become high during the desorption process of shale gas.The reason for this phenomenon is probably due to the main adsorption/desorption of shale gas and diffusion migration fractionation of isotope.In addition,these variation characteristics of methane and ethane carbon isotope composition of shale gas may be the important reason for the low carbon isotopic composition of methane relative to the thermal evolution degree of source rock,and it can be applied to evaluate the amount of remaining resources of shale gas and the fracturing effect.
     
  • CAO Tao-tao,SONG Zhi-guang,WANG Si-bo,XIA Jia
    Natural Gas Geoscience. 2015, 26(2): 341-351. https://doi.org/10.11764/j.issn.1672-1926.2015.02.0341
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    Nitrogen adsorption and mercury intrusion experiments were carried out to study the shale reservoir physical property characteristics and to analyze the controlling factors of Permian shales from well Changcan 1 in Wuhu area in the Lower Yangtze Platform.The results show that the specific surface area is ranging from 4.70m2/g to 21.86m2/g,of which 81.80% is contributed by micropores.The porosities range between 1.18% and 4.95% with most below 4%,and 66.38% of the porosities are from the contribution of mesopores and macropores(crack pores).The permeability is between 0.001×10-3μm2 and 15.56×10-3μm2.Through analyzing the controlling factors,the following conclusions can be drawn:(1)TOC content is the major controlling factor of the specific area for Permian shales|(2)The porosity has an obvious decrease trend with the increase of  TOC content,which may be caused by the isolation and poor connectivity of organic pores with cracks even related to the filling of mineral pore space by organic matter.Micropore and transition-pore volumes have good positive correlation with mineral matter content,while,mesopore and macropore(crack pore)volume has a positive correlation with brittle mineral content|(3)Permeability exhibits an exponential negative correlation with threshold pressure,reflecting the lower the threshold pressure,the higher the permeability and the more beneficial for shale gas production.
  • LI Lei,WANG Xiao-gang,CHEN Ling-ling,TAN Zhuo,CAO Bing,SHEN Wen-long
    Natural Gas Geoscience. 2015, 26(2): 352-359. https://doi.org/10.11764/j.issn.1672-1926.2015.02.0352
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    Ancient tidal channel systems have been recognized and studied by many researchers and constitute an important target for sedimentary study and oil and gas exploration and development.Based on X-drilling data,logs,and 3-D seismic data of Xihu Sag,using facies analysis,seismic forward modeling,seismic attribute analysis and three dimensional imaging technology,the complex tidal channel of Eocene Pinghu Formation was identified and its internal structure,external morphology,stacked style and evolution were studied.Three main conclusions were made:(1)tidal channels were northwest trending,500-1 000m wide and 2-10m deep.Flood and ebb currents could cause tidal channel meanders to laterally migrate and form point bars|(2)tidal channels were composed of eight sedimentary cycles: channel lag deposits-point bar-mud flat-coal marsh or point bar-mud flat-coal marsh.Marine regression was indicated by the fining-upward sequence in a single depositional cycle|(3)within the complex tidal channel system the seismic waveforms,amplitude,and frequency are different from those of the surrounding rock.
     
  • TIAN Ren-fei,YANG Chun-feng,HU Yu,YANG Zhen-feng,LI Qiu-ju
    Natural Gas Geoscience. 2015, 26(2): 360-366. https://doi.org/10.11764/j.issn.1672-1926.2015.02.0360
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    Lithologic reservoir resources are rich in Carboniferous near the top of the Paleogene Chepaizi area,Junggar Basin.But due to the impact of strong amplitude in Carboniferous and limited resolution of seismic data,the conventional seismic attributes cannot effectively portray the vertical and horizontal distribution of the reservoirs.For this issue,spectral decomposition techniques are used to identify thin lithologic reservoirs in the study area.Improved general S transform spectral decomposition techniques are used to perform frequency division of seismic data.Combined with results of a comprehensive analysis,such as the fine horizon calibration of existing drilling data,logging presentation and log interpretation,the 70Hz frequency division section is preferred for reservoir prediction.Results of reservoir prediction are consistent very well with the existing drilling data.They are used to deploy the evaluation well C55-1,which has obtained industrial oil.This further shows that spectral decomposition techniques are effective reservoir exploration techniques in the region with Paleogene Formations and can also be used for thin lithologic reservoirs in other areas.
     
  • WANG Bin,YONG Xue-shan,PAN Jian-guo,TENG Tuan-yu,YIN Lu,XU Duo-nian,HUANG Yu,KONG Xu
    Natural Gas Geoscience. 2015, 26(2): 367-370. https://doi.org/10.11764/j.issn.1672-1926.2015.02.0367
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    It suggests that the shale gas content,regardless of the free gas or the adsorbed one,increases with the formation pressure.Therefore,it is of significance to carry out the fine formation pressure forecast to improve the shale gas production.Current studies on the pressure forecast are mainly based on the fact that the P-wave velocity decreases with the increasing formation pressure.The P-wave velocity change,however,depends not just on the formation pressure change.So in order to build a high-precision forecast model of the formation pressure,we start with the definition of the Young′s and Bulk modulus,deduce the relationship between the effective stress and the Vp and Vs  combined with the wave equation,and develop a new forecast method,Elastic Parameters Combination,to calculate the formation pressure.By introducing the S-wave velocity,this method reduces the multiplicity of the pressure forecast,improves the accuracy,and demonstrates its effectiveness through the application on the shale gas strata.
     
  • SONG Lian-teng,LIU Zhong-hua,LI Chao-liu,YUAN Chao
    Natural Gas Geoscience. 2015, 26(2): 371-376. https://doi.org/10.11764/j.issn.1672-1926.2015.02.0371
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    The causes of abnormal pressure are complex and also have different calculation methods.In practical applications,if the cause of abnormal pressure is not been fully aware,it can lead to serious errors.According to the cause of abnormal pressure in the study area,we chose Bowers method to process and analyze well Y in Dagang Oilfield and then found that the actual MDT test pressures were different from that calculated by Bowers method,this abnormal pore pressure has not been reported in the domestic oil fields.For this exception,on basis of the data collection and literature research,we analyze the pressure causes for the first time.We confirm the causes by using field research which is correct.This also shows that considering the causes of pore pressure calculation method is necessary and important on the other hand.Meanwhile,this also provides a train of thought for using pore pressure data to invert causes.
  • TIAN Wei,ZHU Wei-yao,ZHU Hua-yin,ZHANG Xue-ling,WANG Rui-ming,LI Yong
    Natural Gas Geoscience. 2015, 26(2): 377-383. https://doi.org/10.11764/j.issn.1672-1926.2015.02.0377
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    In order to seek for a set of reasonable measurement method for evaluation of back pressure stress sensitivity,current national standards are analyzed and the deficiencies are pointed out.The results show that the current national standard is not concrete although it is advanced compared with the original standard.It demands a constant confining pressure during the measurement process,but did not mention how to control the inlet pressure.The experiment simulated reservoir conditions well.According to the national standard definition for the net confining pressure and net stress,it can be speculated that inlet pressure changed with the changes of back pressure,but there is no confinement for pressure differential between upstream and downstream.A simple experiment is designed for inner pressure,it indicates the measurement process is simultaneously affected by the confining pressure and the back pressure.The current exploration are mostly devoted to the back pressure stress sensitivity considering the inner pressure changes,but it cannot well simulate the actual development process of gas reservoir.The actual situation is that the effective stress increases in the near oil wellbore area as the production well bottom pressure decreases,and extend into far wellbore area.This trend becomes weaker from the near to the distant due to the existence of pressure drop funnel.Based on the above analysis,a new set of measurement method for back pressure stress sensitivity is established,which required a constant confining pressure and upstream pressure.These pressure should equal to the overlying pressure and the original reservoir pressure of the actual reservoir respectively.The back pressure decreases from the original reservoir pressure to abandonment pressure points,which simulates the back pressure reduction process in the actual gas reservoirs development.The permeability is measured under different back pressure.This method is applied to measure the permeability of tight sandstone in Tuha oil field.The result shows that the permeability variation amplitude is about 21%,and the sensitivity degree is weak.The experimental permeability change rate curve is divided into steep section and gentle section,and a inflection point obviously existed.The measurement results agree well with expectations,so this new method can be applied to future tests and scientific research.
     
     
  • XIE Wei-yang,LI Xiao-ping,ZHANG Lie-hui,WANG Jun-chao,CHENG Zi-yang,YUAN Lin
    Natural Gas Geoscience. 2015, 26(2): 384-390. https://doi.org/10.11764/j.issn.1672-1926.2015.02.0384
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    Shale gas reservoirs can get industrial gas flow now due to the technical progress of horizontal well drilling and hydraulic fracturing.Based on the special flow mechanism and desorption phenomenon of shale gas reservoir,this paper presents a transient analysis model of multi-stage fractured horizontal well with the consideration of wellbore storage,skin effect and hydraulic fractures parameters of shale gas reservoirs.Accurate solution to this flow model was obtained by the use of source function theory,Laplace transform,three-dimensional eigenvalue method and orthogonal transformation.Production decline type curves were plotted by using the Stehfest algorithm.Seven different flow regimes were identified.The effects of influence factors such as skin coefficient,absorption index,fractures number,horizontal well length and fracture permeability were discussed.This research could be used to interpret the production decline behavior more accurately and effectively for shale gas reservoirs.

  • WEI Wei,GUO Kang-liang,TIAN Lang,HE Liang,CHEN Kai-yan
    Natural Gas Geoscience. 2015, 26(2): 391-396. https://doi.org/10.11764/j.issn.1672-1926.2015.02.0391
    Abstract ( ) Download PDF ( )   Knowledge map   Save
    In deliverability evaluation of oil and gas field,the single point deliverability equation and binomial deliverability equation are often used to obtain the productivity to strike open flow capacity.For some special cases of the well,pressure gauge can not be put into the middle layer,conventional methods require the wellhead pressure converted into bottom-hole pressure,then find the binomial deliverability equation and single point deliverability equation suitable for the area,this is not only time consuming but also increases the uncertainty.In this paper,based on the data of TWT Gasfield,we try to directly use wellhead pressure to obtain the wellhead productivity equation but not through convert wellhead pressure.Compared to the open flow capacity derived from wellhead productivity equation and conventional deliverability equation,it is found to have the function very well,thus verify the feasibility of the method that does not convert wellhead pressure but directly calculate wellhead productivity equation and absolute open flow capacity by wellhead pressure.