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Article Navigation >  Acta Sedimentologica Sinica  > 2002  >  20(2): 222-228

YANG MingHui, LIU ChiYang. Types, Textures and Series of the Continental Sequences and Model of Sedimentary Basin-Fill in Rift Basin: A Case Study from Jizhong Basin, China[J]. Acta Sedimentologica Sinica, 2002, 20(2): 222-228.
Citation: YANG MingHui, LIU ChiYang. Types, Textures and Series of the Continental Sequences and Model of Sedimentary Basin-Fill in Rift Basin: A Case Study from Jizhong Basin, China[J]. Acta Sedimentologica Sinica, 2002, 20(2): 222-228.
shu

Types, Textures and Series of the Continental Sequences and Model of Sedimentary Basin-Fill in Rift Basin: A Case Study from Jizhong Basin, China

  • 1.

    Basin & Reservoir Research Center,University of Petroleum,Beijing 102249;

  • 2.

    2 Department of Geology,Northwest University,Xi'an 710069

  • Received Date: 2001-05-14
  • Rev Recd Date: 2001-08-09
  • Publish Date: 2002-04-10
  • The continental sequence deeply affected by natural geographic districts, geological forces and strata types, therefore occurred some kinds of types. There are three kinds of sequence types including alluvial sequence, lacustrine sequence and fluvial sequence that present in Jizhong basin during the syn extensional stage. The alluvial sequence is mainly composed of alluvial fan systems and grows up in the initial stages of the basin development. Here the relief contrast was strong, provenance supply was abundant and climate was arid, so the lacustrine area was narrow in proportion to the alluvial and fluvial area. The lacustrine sequence mainly made up of lacustrine sedimentary systems, and partially fluvial sediments and a little of alluvial interlayer. The stage was a period of rapid growth of the rift basin. The basin base subsidized fast and climate humid, lacustrine area larger, thereby gaining a period for hydrocarbon rock to form. The fluvial sequence began to form in last stage of the basin extend. The geographic contrast gradually was reduced. The deposit was far from the source region,and the area of the fluvial systems was deadly larger than the area of the lacustrine. The authors suggested that a polynomial relation exists between the lake level change and tectonic movement, provenance, climate factor and so on, the former only incarnates the synthetically changes of the latter. The sequence texture of the continental rift basin is under the control of the lake level change, like the sequence texture of the marine basin is controlled by sea level change. Therefore, the continental sequence may be trisection according to the lake level change. The sequences of the continental rift basin controlled by tectonic movement develop in succession, as the alluvial sequence located at the bottom, the lacustrine sequence at the middle and the fluvial sequence at the upper. This serial sequences is a response that sedimentary basin fill to the episodic tectonic movement. During the basin fill, there is clearly a difference among the sedimentary system tract growth of each sequence. In general, the lowstand system tract (LST) of the alluvial sequence is superior to the lacustrine and fluvial sequences. The LST of the lacustrine is absent and/or lack, but the transgressive system tract (TST) and/or highstand system tract (HST) deposited in the lake level rise are best of all development. The LST and/or HST deposited in the lake level fall of the fluvial sequence are the best in the each sequence. The tectonic movement is primary factor to control the continental sequence type, and the lake level change controls the texture of the sequences.
  • [1] 1. Vail P R,Mitchum R M,Thompson S.Seismic stratigraphy and global changes of sea level,part three:relative changes of sea level from coastal onlap[C].AAPG Memoir 26,1977.63～82

    2. Van Wagoner J C,Mitchum R M,Campion K M,et al.Siliciclastic sequence stratigraphy in well logs,cores and outcrops: concepts for high-resolution correlation of time and facies[C].AAPG,Methods in Exploration Series 7,1990,55:1～240

    3. 夏文臣，雷建喜，周杰。成因地层分析的思路与方法[J].煤田地质与勘探，1991,19（4）:1～9 [Xai Wenchen,Lei Jianxi,Zhou Jie.Through and method of genetic stratigraphic analysis[J].Coal Geology Exploration,1991,19（4）:1～9]

    4. 李思田，林畅松，解习农等。大型陆相盆地层序地层学研究[J].地学前缘，1995,2（4）:133～136 [Li Sitian,Lin Changsong,Xie Xinong,et al.Approaches of nonmarine sequence stratingraphy--a case study on the Mesozoic Ordos basin[J].Earth Science Fronties,1995,2（4）:133～136]

    5. 王东坡，刘立。大陆裂谷盆地层序地层研究[J].岩相古地理，1994,14（3）:1～9 [Wang Dong-po,Liu Li.Sequence stratigraphy of continetal rift basin[J].Sedimentary facies and Paleogeography,1994,14（3）:1～9]

    6. 顾家裕。陆相盆地层序地层学格架概念及模式[J].石油勘探与开发，1995,22（4）:6～10 [Gu Jiayu.Framework concepts and models of sequence stratigraphy in nonmarine petrolferous basin[J].Petroleum Exploration and Development,1995,22（4）:6～10]

    7. Wright V A.The sequence stratigraphy of fluvail depositional system:the role of floodplain sediment storage[J].Sedimentary Geology,1993,86（2）:203～210

    Shanley K W,McCabe P J.Perspective on the sequence stratigraphy of continental [J].AAPG Bull.,1994,78（4）:544～568

    8. 程日辉，刘招君，王东坡。陆相盆地充填层序的类型-以辽西地区中生代盆地为例[J].沉积学报，1997,15（3）:166～170 [Cheng Rihui,Liu Zhaojun,Wang Dongpo.Types of filling sequences in in continental basins-examples from Mesozoic basins basins,western Liaoning Province[J].Acta Sedimentologica Sinica,1997,15（3）:166～170]

    9. Cross T A.High-resolution stratigraphic correlation from the perspective of base-level cycles and sediment accommodation [C].In: Proceeding of Northwestern European Sequence Stratigraphy Congress,1994.105～123

    10. Olsen P E.Tectonic,climatic and biotic modulation of lacustrine ecosystems-examples from Newark supergroup of eastern North America[C].AAPG Memoir 50,1991:209～224

    11. 邓宏文。美国层序研究中的新学派-高分辨率层序地层学[J].石油与天然气地质，1995,16（2）:89～97 [Deng Hongwen.A new school of through in sequence stratigraphic studies in U.S.:high resolution sequence stratigraphy[J].Oil Gas Geology,1995,16（2）:89～97]

    12. 邬金华，毛志超，张哲。河相层序地层研究进展述评[J].地质科技情报，1997,16（3）:40～46 [Wu Jinhua,Mao Zhichao,Zhang Zhe.Review of the development of fluvial sequence stratigraphy[J].Geological Science and Technology Information,1997,16（3）:40～46]

    13. 魏魁生，徐怀大。二连盆地白垩系非海相沉积层序地层特征[J].地球科学，1994,19（2）:181～193 [Wei Kuisheng,Xu Huaida.Sequence stratigraphic features of Cretaceous nonmarine sediments in Erlian basin[J].Earth Science,1994,19（2）:181～193]

    14. 解习农，李思田。陆相盆地层序地层研究特点[J].地质科技情报，1993,12（1）:22～26 [Xie Xiong,Li Sitian.The characteristic of sequence stratigphy in nonmarine basin[J].Geological Science and Technology Information,1993,12（1）:22～26]

    15. 徐怀大。层序地层学理论用于我国断陷盆地分析中的问题[J].石油与天然气地质，1991,55（4）:52～87 [Xu Huaida.Problems in analysis of faulted basins of China based on sequence stratigraphic theory[J].Oil Gas Geology,1991,12（1）:52～57]

    16. 魏魁生，徐怀大。冀中坳陷早第三纪海泛特征及其层序地层学意义[J].现代地质，1993,7（3）:274～283 [Wei Kusheng,Xu Huaida Marine inundation feature and its significance of sequence stratigraphy of Eogene in central Hebei[J].Geoscience,1993,7（3）:274～283]

    17. 胡受权，颜其彬。试论泌阳断陷双河-赵凹地区下第三系核三上段陆相层序中岩石地球化学旋回性特征[J].地球化学，1999,28（1）:87～96 [Hu Shouquan,Yan Qibin.Lithologic-geochemical cyclitity in terrigenous sequence of the Upper member of Eh in Shuanghe-Zhaoao,Biyang fault depression[J].Geochimica,1999,28（1）:87～96]

    18. 岳文浙，丁保良，魏乃颐。陆盆层序地层研究的思路[J].地质论评，2000,46（4）:347～353 [Yue Wenzhen,Ding Baoliang,Wei Naiyi.Thoughts on the study of continental sequence stratigraphy[J].Geological Review,2000,46（4）:374～354]

    19. Scholz C A,Rosendahl B R.Corase-clastic facies and stratigraphic sequence models from lakes Malawi and Tanganyika,East Africa[C].AAPG Memoir 50,1991:151～168

    20. 杨明慧，夏文臣。非海相前陆盆地含煤沉积层序地层分析[J].煤田地质与勘探，1998,26（3）:1～4 [Yang Minghui,Xia Wenchen.The sequence stratigraphic analysis of coal-bearing srata in nonmarine foreland basin[J].Coal Geology Exploration,1998,26（3）:1～4]

    21. Oslen T,Steel R H,Gseth K,et al.Sequential architecture in a fluvial succession: sequence stratigraphy in the Upper Cretaceous Mesaverde Group,Prince Canyon,Utah[J].Journal of Sedimentary Research,1995,865（2）:265～280

    22. 李思田等。鄂尔多斯盆地东北部层序地层学及沉积体系分析[M].北京:地质出版社，1992 [Li Sitian,Cheng Shoutian,Yang Shigong,et al.Sequence stratigraphy and development system analysis of the Northeastern Ordos Basin[M].Beijing:Geological Publishing House,1992]
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  • Received:  2001-05-14
  • Revised:  2001-08-09
  • Published:  2002-04-10

Types, Textures and Series of the Continental Sequences and Model of Sedimentary Basin-Fill in Rift Basin: A Case Study from Jizhong Basin, China

  • 1. Basin & Reservoir Research Center,University of Petroleum,Beijing 102249;
  • 2. 2 Department of Geology,Northwest University,Xi'an 710069
  • Received Date: 2001-05-14
  • Rev Recd Date: 2001-08-09
  • Publish Date: 2002-04-10

Abstract: The continental sequence deeply affected by natural geographic districts, geological forces and strata types, therefore occurred some kinds of types. There are three kinds of sequence types including alluvial sequence, lacustrine sequence and fluvial sequence that present in Jizhong basin during the syn extensional stage. The alluvial sequence is mainly composed of alluvial fan systems and grows up in the initial stages of the basin development. Here the relief contrast was strong, provenance supply was abundant and climate was arid, so the lacustrine area was narrow in proportion to the alluvial and fluvial area. The lacustrine sequence mainly made up of lacustrine sedimentary systems, and partially fluvial sediments and a little of alluvial interlayer. The stage was a period of rapid growth of the rift basin. The basin base subsidized fast and climate humid, lacustrine area larger, thereby gaining a period for hydrocarbon rock to form. The fluvial sequence began to form in last stage of the basin extend. The geographic contrast gradually was reduced. The deposit was far from the source region,and the area of the fluvial systems was deadly larger than the area of the lacustrine. The authors suggested that a polynomial relation exists between the lake level change and tectonic movement, provenance, climate factor and so on, the former only incarnates the synthetically changes of the latter. The sequence texture of the continental rift basin is under the control of the lake level change, like the sequence texture of the marine basin is controlled by sea level change. Therefore, the continental sequence may be trisection according to the lake level change. The sequences of the continental rift basin controlled by tectonic movement develop in succession, as the alluvial sequence located at the bottom, the lacustrine sequence at the middle and the fluvial sequence at the upper. This serial sequences is a response that sedimentary basin fill to the episodic tectonic movement. During the basin fill, there is clearly a difference among the sedimentary system tract growth of each sequence. In general, the lowstand system tract (LST) of the alluvial sequence is superior to the lacustrine and fluvial sequences. The LST of the lacustrine is absent and/or lack, but the transgressive system tract (TST) and/or highstand system tract (HST) deposited in the lake level rise are best of all development. The LST and/or HST deposited in the lake level fall of the fluvial sequence are the best in the each sequence. The tectonic movement is primary factor to control the continental sequence type, and the lake level change controls the texture of the sequences.

YANG MingHui, LIU ChiYang. Types, Textures and Series of the Continental Sequences and Model of Sedimentary Basin-Fill in Rift Basin: A Case Study from Jizhong Basin, China[J]. Acta Sedimentologica Sinica, 2002, 20(2): 222-228.
Citation: YANG MingHui, LIU ChiYang. Types, Textures and Series of the Continental Sequences and Model of Sedimentary Basin-Fill in Rift Basin: A Case Study from Jizhong Basin, China[J]. Acta Sedimentologica Sinica, 2002, 20(2): 222-228.
shu

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