Barrier Island and Its Genesis Analysis of Xiaotangzi Formation  of Upper Triassic in Central Sichuan Basin

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  • 1.China University of Mining and Technology (Beijing), Beijing 100083, China;
    2.Research Institute of Petroleum Exploration and Development-Langfang, PetroChina, Langfang 065007, China

Received date: 2012-06-04

  Revised date: 2012-08-13

  Online published: 2019-01-08

Abstract

Barrier island is not only important for human residence,but also an important oil and gas accumulation unit.By the shore seaward,barrier dam and marshes,tidal flats,lagoons and shallow continental shelf accompanied each other,some areas of the coastal developed small delta.From the bottom,the shallow continental shelf,tidal channel,swamp and lagoon sedimentary facies constitute a complete sedimentary cycle in vertical.The barrier dam formation was related to the sea level rise,the small slope of the terrain,the development of terrain slope break belt and stability sandy source supply.Stable sea level rise and wave transformation formed terrain slope break belt near the body of a long strip of sand in the subtidal area.Small terrain slope is conducive to the gradually weaken of wave and tidal energy,and the sandy sediments gradual accumulated near the twists.With the continue arise of sea level,stable supply of sandy material source can ensure,the barrier dam to grow and not be submerged.

Cite this article

JIN Hui, SHI Zhen-sheng, YANG Wei, SHEN Jue-hong . Barrier Island and Its Genesis Analysis of Xiaotangzi Formation  of Upper Triassic in Central Sichuan Basin[J]. Natural Gas Geoscience, 2013 , 24(1) : 19 -28 . DOI: 10.11764/j.issn.1672-1926.2013.01.19

References



[1]Davis Jr  R A,Yale K E,Pekala J M,et al.Barrier island stratigraphy and Holocene history of west-central Florida[J].Marine Geology,2003,200:103-123.

[2]Rosati J D,Dean R G,Stone G W.A cross-shore model of barrier island migration over a compressible substrate[J].Marine Geology,2010,271:1-16.

[3]Dickenson W R.Provenance and sediment dispersal in relation to paleotectonics and paleogeography of sedimentary basins[M]//Kleinspeshn K L,Paola C,eds.New Perspectives in Basin Analysis.New York: Speringer-Verlag,1988:3-26.

[4]Dickinson W R,Suczek C A.Plate tectonics and sandstone compositions[J].AAPG Bulletin,1979,63(12):2164-2182.

[5]Galloway W E,Hobday D K.Terrigenous Clastic Depositional Systems:Applications to Petroleum,Coal,and Uranium Exploration[M].Berlin: Springer,1984.

[6]Hodgkinson J,Cox M E,Mcloughlin S,et al.Lithological heterogeneity in a back-barrier sand island: Implication for modlling hydrogeological frameworks[J].Sedimentary Geology,2008,203:64-86

[7]Hine A C,Evans M W,Davis R A,et al.Depositional response to seagrass mortality along a low-energy,barrier-island coast: West-central florida[J].Journal of Sedimentary Petrology,1987,57:431-439

[8]Zhong Guangfa,Hou Fanghao.Sedimentary systems and generation potential of hydrocarbon in No 1 Member of late Triassic Xujiahe Formation,northwest Sichuan[J].Journal of Jianghan Petroleum Institute,1992,14(1):16-22.[钟广法,侯方浩.川西北上三叠统须一段沉积体系及生烃潜力[J].江汉石油学院学报,1992,14(1):16-22.]

[9]Shi Zhensheng,Zhao Zhengwang,Jin Hui,et al.Depositional systems and its geological significance of Xiaotangzi Formation of late Triassic Sichuan basin[J].Journal of Palaeogeography,2012,14(4):477-486.[施振生,赵正望,金惠,等.四川盆地上三叠统小塘子组沉积特征及地质意义[J].古地理学报,2012,14(4):477-486.]

[10]Zhang Zhongwu.Oil and gas containing structures and evolution of Sichuan basin[M]//Oil and Gas Containing Tectonics in China.Beijing: Petroleum Industry Press,1989:211-228.[张仲武.四川盆地含油气构造特征及评价[M]//中国含油气区构造特征.北京:石油工业出版社,1989:211-228.]

[11]Wu Xichun,Zhang Liangjian.Late Triassic (Carnian) sponge patchreefs in northwestern Sichuan basin[J].Geological Science,1982,(4):385-389.[吴熙纯,张亮鉴.四川盆地西北部晚三叠世卡尼期的海绵斑块礁[J].地质科学,1982,(4):385-389.]

[12]Wu Xichun.Paleoecological characteristics of late Triassic sponge patch reefs in north-western Sichuan,China[J].Acta Palaeontologica Sinica,1984,29(3):349-365.[吴熙纯.川西北晚三叠世的海绵动物群[J].古生物学报,1984,29(3):349-365.]

[13]Zhang Jian,Li Guohui,Xie Jirong,et al.Stratigraphic division and correlation of upper Triassic in Sichuan basin[J].Natural Gas Industry,2006,26(1):12-16.[张健,李国辉,谢继容,等.四川盆地上三叠统划分对比研究[J].天然气工业,2006,26(1):12-16.]

[14]Deng Kangling,He Li,Qin Dayou,et al.The earlier late Triassic sequence and its sedimentary environment in western Sichuan basin[J].Oil & Gas Geology,1982,3(3):204-210.[邓康龄,何鲤,秦大有,等.四川盆地西部晚三叠世早期地层及其沉积环境[J].石油与天然气地质,1982,3(3):204-210.]

[15]Yang Jikai.Found of late Triassic bryozoan fossil in northwest Sichuan[J].Journal of Chengdu College of Geology,1979,(4):84-90.[杨季楷.川西北晚三叠世苔藓虫化石的发现[J].成都地质学院学报,1979,(4):84-90.]

[16]Gou Zonghai.New materials of fossil shells of early Late Triassic in Maantang area,Jiangyou county of Sichuan[J].Journal of Chengdu College of Geology,1980,(1):105-107.[苟宗海.四川江油县马鞍塘地区晚三叠世早期瓣鳃化石新材料[J].成都地质学院学报,1980,(1):105-107.]

[17]Sun Yuxian,Yang Jikai.Found of carnian calcareous algae in late Triassic northwest Sichuan[J].Journal of Chengdu College of Geology,1980,(1):101-104.[孙玉娴,杨季楷.川西北晚三叠世卡尼期钙藻的发现[J].成都地质学院学报,1980,(1):101-104.]

[18]Duan Lilan.Some late Triassic(Carnian) scleractinia from northwest Sichuan[J].Journal of Chengdu College of Geology,1983,(2):48-58.[段丽兰.川西北晚三叠世卡尼期的硬珊瑚[J].成都地质学院学报,1983,(2):48-58.]

[19]Wang Yunsheng.The earlier late Triassic Ammonites from Longmen mountains[J].Journal of Chengdu College of Geology,1992,19(4):28-35.[王运生.龙门山晚三叠世早期菊石[J].成都地质学院学报,1992,19(4):28-35.]

[20]Shi Zhensheng,Yang Wei,Xie Zengye,et al.Upper Triassic clastic composition in Sichuan basin,southwest China:Implication for provenance analysis and the Indosinian orogeny[J].Acta Geologica Sinica,2010,84(3):387-397.[施振生,杨威,谢增业,等.四川盆地晚三叠世碎屑组分对源区分析及印支运动的指示[J].地质学报,2010,84(3):387-397.]

[21]Shi Zhensheng,Wang Xiuqin,Wu Changjiang.The heavy minerals and provenances of the upper Triassic Xujiahe Formation in Sichuan basin[J].Natural Gas Geoscience,2011,22(4):618-627.[施振生,王秀芹,吴长江.四川盆地上三叠统须家河组重矿物特征及物源区意义[J].天然气地球科学,2011,22(4):618-627.]

[22]Shi Zhensheng,Yang Wei.Genesis of widespread sandbodies of upper Triassic in Sichuan basin[J].Acta Sedimentologica Sinica,2011,29(6):1058-1068.[施振生,杨威.四川盆地上三叠统砂体大面积分布的成因[J].沉积学报,2011,29(6):1058-1068.]

[23]Dickinson K A,Berryhill Jr H L,Holmes C W.Criteria for recognizing ancient barrier coastlines[M].Rigby J K,Hamblin W K,Eds.Recognition of Ancient Sedimentary Environments.SEPM Special Publication,1972:192-214.

[24]Jia Dong,Chen Zhuxin,Jia Chengzao,et al.Structural features of the Longmen Shan fold and thrust belt and development of the western Sichuan foreland basin,central China[J].Geological Journal of China University,2003,9(3):462-469.[贾东,陈竹新,贾承造,等.龙门山褶皱冲断带构造解析与川西前陆盆地的发育[J].高校地质学报,2003,9(3):462-469.]

[25]Wang Hongjun,Bian Congsheng,Shi Zhensheng.The control effect of effective source reservoir combinations to gas reservoir formation in Xujiahe Formation,Sichuan basin[J].Natural Gas Geoscience,2011,22(1):38-46.[王红军,卞从胜,施振生.四川盆地须家河组有效源储组合对天然气藏形成的控制作用[J].天然气地球科学,2011,22(1):38-46.]

[26]Dai Chaocheng,Zheng Rongcai,Zhu Rukai,et al.Reservoir characteristics of the Xujiahe Formation in central-west Sichuan analogous foreland basin[J].Natural Gas Geoscience,2011,22(1):47-55.[戴朝成,郑荣才,朱如凯,等.四川类前陆盆地中西部须家河组储层特征[J].天然气地球科学,2011,22(1):47-55.]

[27]Rautman C A.Sedimentology of late Jurassic barrier-island complex,lower Sundance Formation of black hills[J].AAPG  Bulletin,1978,62(11):2275-2289.

[28]Stephen P L,Michael R R,John E S.Barrier island evolution in response to sea level rise:Discussion and reply[J].Journal of Sedimentary Research,1983,53(3):1026-1033.

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