Natural Gas Geoscience ›› 2023, Vol. 34 ›› Issue (1): 96-110.doi: 10.11764/j.issn.1672-1926.2022.09.008
Previous Articles Next Articles
Chengsheng CHEN1,2(),Rui DENG1,2,Haizu ZHANG3,Yunpeng WANG1,2()
CLC Number:
1 | 杨海军,陈永权,田军,等.塔里木盆地轮探1井超深层油气勘探重大发现与意义[J].中国石油勘探,2020,25(2):62-72. |
YANG H J,CHEN Y Q,TIAN J,et al.An important discovery in Well Luntan-1 of the Tarim Basin, China, and its significance for ultra-deep oil and gas exploration[J].China Petroleum Exploration,2020,25(2):62-72. | |
2 | 王招明,谢会文,陈永权,等.塔里木盆地中深1井寒武系盐下白云岩原生油气藏的发现与勘探意义[J].中国石油勘探,2014,19(2):1-13. |
WANG Z M,XIE H W,CHEN Y Q,et al.Discovery and exploration of Cambrian subsalt dolomite original hydrocarbon reservoir at Zhongshen-1 Well in Tarim Basin[J].China Petroleum Exploration,2014,19(2):1-13. | |
3 | 张纪智,王招明,杨海军,等.塔里木盆地中深地区寒武系盐下白云岩油气来源及差异聚集[J].石油勘探与开发,2017,44(1):40-47. |
ZHANG J Z,WANG Z M,YANG H J,et al.Origin and differential accumulation of hydrocarbons in Cambrian sub-salt dolomite reservoirs in Zhongshen area,Tarim Basin,NW China[J].Petroleum Exploration and Development,2017,44(1):40-47. | |
4 | 朱光有,胡剑风,陈永权,等.塔里木盆地轮探1井下寒武统玉尔吐斯组烃源岩地球化学特征与形成环境[J].地质学报,2022,96(6):1-16. |
ZHU G Y,HU J F,CHEN Y Q,et al.Geochemical characteristics and formation environment of source rock of the Lower Cambrian Yuertusi Formation in Well Luntan 1 in Tarim Basin[J].Acta Geologica Sinica,2022,96(6):1-16. | |
5 | CHEN C S,WANG Y P,BEAGLE J R,et al.Reconstruction of the evolution of deep fluids in light oil reservoirs in the central Tarim Basin by using PVT simulation and basin modeling[J].Marine and Petroleum Geology,2019,107:116-126. |
6 | HUANG H P,ZHANG S C,SU J.Palaeozoic oil-source correlation in the Tarim Basin, NW China: A review[J].Organic Geochemistry,2016,94:32-46. |
7 | ZHU G Y,CHEN F R,WANG M.et al.Discovery of the lower Cambrian high-quality source rocks and deep oil and gas exploration potential in the Tarim Basin, China[J].AAPG Bulletin,2018,102(10):2123-2151. |
8 | 杨海军,于双,张海祖,等.塔里木盆地轮探1井下寒武统烃源岩地球化学特征及深层油气勘探意义[J].地球化学,2020,49(6):666-682. |
YANG H J,YU S,ZHANG H Z,et al.Geochemical characteristics of Lower Cambrian sources rocks from the deepest drilling of Well LT-1 and their significance to deep oil gas exploration of the Lower Paleozoic system in the Tarim Basin[J].Geochimica,2020,49(6):666-682. | |
9 | 彭平安,贾承造.深层烃源演化与原生轻质油/凝析油气资源潜力[J].石油学报,2021,42(12):1543-1555. |
PENG P A,JIA C Z.Evolution of deep source rock and resource potential of primary light oil and condensate[J].Acta Petrolei Sinica,2021,42(12):1543-1555. | |
10 | DENG R,CHEN C S,SHI S Y,et al.Fluid phase simulation and evolution of a condensate gas reservoir in the Tazhong Uplift, Tarim Basin[J].Geofluids,2019,8627698. |
11 | TAN J Q,HORSFIELD B,MAHLSTEDT N,et al.Physical properties of petroleum formed during maturation of Lower Cambrian shale in the Upper Yangtze Platform, South China, as inferred from PhaseKinetics modelling[J].Marine and Petroleum Geology,2013,48:47-56. |
12 | PRIMIO R D,HORSFIELD B.From petroleum-type organofacies to hydrocarbon phase prediction[J].AAPG Bulletin,2006,90(7):1031-1058. |
13 | ABBASSI S,EDWARDS D S,GEORGE S C,et al.Petroleum potential and kinetic models for hydrocarbon generation from the Upper Cretaceous to Paleogene Latrobe group coals and shales in the Gippsland Basin, Australia[J].Organic Geochemistry,2016,91:54-67. |
14 | 徐杰, 李涛, 陈国光, 等.塔里木盆地轮南潜山构造特征[J].石油学报,2002,23(5):14-18. |
XU J,LI T,CHEN G G,et al.Structural features of the buried hill in Lunnan area of Tarim Basin[J].Acta Petrolei Sinica,2002,23(5):14-18. | |
15 | 张云鹏,任建业,阳怀忠,等.塔里木盆地轮南低凸起构造特征及演化[J].石油与天然气地质,2011,32(3):440-447. |
ZHANG Y P,REN J Y,YANG H Z,et al.Structure features and its evolution of Lunnan low uplift of the Tarim Basin[J].Oil & Gas Geology,2011,32(3):440-447. | |
16 | 陈承声,史树勇,王云鹏.基于PetroMod四川盆地长宁地区五峰—龙马溪组优质页岩段吸附模拟研究[J].地球化学,2019,48(6):602-612. |
CHEN C S,SHI S Y,WANG Y P.Adsorption simulation based on PetroMod of high-quality shale segment of Wufeng-Longmaxi Formation in Changning area, Sichuan Basin[J].Geochimica,2019,48(6):602-612. | |
17 | BURGREEN-CHAN B,GRAHAM S A.Petroleum system modeling of the East Coast Basin, Hawke Bay, New Zealand[J].AAPG Bulletin,2018,102(4):587-612. |
18 | KAUERAUF A I, HANTSCHEL T.Fundamentals of Basin and Petroleum Systems Modeling[M].Berlin, Heidelberg:Springer-Verlag,2009. |
19 | TORSVIK T H,COCKS L R M.Chapter 2 new global palaeogeographical reconstructions for the Early Palaeozoic and their generation[M]// HARPER D A T, SERVAIS T.Early Palaeozoic Biogeography and Palaeogeography.Memoirs 38.London: The Geological Society of London,2013:5-24. |
20 | SCOTESE C R.Late proterozoic plate tectonics and palaeogeography: A tale of two supercontinents, Rodinia and Pannotia[J].Geological Society,2009,326(1):67-83. |
21 | AMBROSE G J,KRUSE P D,PUTNAM P E.Geology and hydrocarbon potential of the southern Georgina Basin, Australia[J].The APPEA Journal,2001,41(1):139-163. |
22 | PRIMIO R D,DIECKMANN V,MILLS N.PVT and phase behaviour analysis in petroleum exploration[J].Organic Geochemistry,1998,29 (1-3):207-222. |
23 | PÉNELOUX A,RAUZT E,FRÉZE R.A consistent correction for Redlich-Kwong-Soave volumes[J].Fluid Phase Equilibria,1982,8(1):7-23. |
24 | PENG D Y,ROBINSON D B.A new two-constant equation of state[J].Industrial and Engineering Chemistry Fundamentals,1976,15(1):59-64. |
25 | LIU D H,XIAO X M,MI J K,et al.Determination of trapping pressure and temperature of petroleum inclusions using PVT simulation software:A case study of Lower Ordovician carbonates from the Lunnan Low Uplift, Tarim Basin[J].Marine and Petroleum Geology,2003,20(1):29-43. |
26 | QIU N S,CHANG J,ZUO Y H,et al.Thermal evolution and maturation of Lower Paleozoic source rocks in the Tarim Basin,northwest China[J].AAPG Bulletin,2012,96(5):789-821. |
27 | ZHU G Y,MILKOV A V,LI J F,et al.Deepest oil in Asia: Characteristics of petroleum system in the Tarim Basin, China[J].Journal of Petroleum Science and Engineering,2021,199:108246. |
28 | DENG R,WANG Y P,CHEN C S.Fluid phase modeling and evolution of complex reservoirs in the Halahatang Depression of the Tabei Uplift, Tarim Basin[J].ACS Omega,2022,7(17):14933-14943. |