The Apparent Types of Sequence Bottom Boundary Surface--Taking marine Sinian System to Middle Triassic Series in South China as an example

TIAN Jing chun; CHEN Hong de; QIN Jian xiong; HOU Ming cai; ZHAO Jun xing

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Article Navigation > Acta Sedimentologica Sinica > 2003 > 21(4): 675-682

TIAN Jing chun, CHEN Hong de, QIN Jian xiong, HOU Ming cai, ZHAO Jun xing. The Apparent Types of Sequence Bottom Boundary Surface--Taking marine Sinian System to Middle Triassic Series in South China as an example[J]. Acta Sedimentologica Sinica, 2003, 21(4): 675-682.

Citation:

The Apparent Types of Sequence Bottom Boundary Surface--Taking marine Sinian System to Middle Triassic Series in South China as an example

State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation Institute of Sedimentology, Chengdu University of Technology, Chengdu 610059

Received Date: 2002-05-31
Rev Recd Date: 2002-09-09
Publish Date: 2003-12-10

Abstract

It is well known that the key of research on sequence stratigraphy is sequence division, but first of all the key of sequence division is identification of boundary surface. The boundary surface of defined sequence included sequence bottom boundary surface first trangressive surface and maximum marine f looding surface. Among them, the most important is bottom boundary surface indentification because it is sequence division foundation. The paper, taking marine Sinian system to Middle Triassic Series in south China as an example, through anlyses of filed geologic sections, identified nine types sequence bottom boundary surfaces which are: ( 1) weathering crust;(2) Paleosol;(3) Erosion surface of river rejuvenation;(4) Action surface of ancient karst;(5) Washing erosion surface of gravity flow on slop;(6) Erosion surface of turbidity flow in basin;(7) Action surface of volcano event;(8) Transition surface of rock character and facies;(9) onlap surface. Research features of above boundary surfaces in detail is very important for sequence division.
- sequence,
- boundary surface,
- apparent type

References

[1]	陈洪德,覃建雄,田景春,等.右江盆地层序充填动力学初探[J].沉积学报,2000,18(2):165～171[Chen Hongde,Qin Jianxiong,Tian Jingchun,et al. Sequence filling dynamics of Youjiang basin,Southern China[J]. Acta Sedimentologica Sinica, 2000,17(4):165～171]
[2]	冯庆来.桂西北早石炭世台槽地区露头层序地层及海平面变化研究[J].地球科学,1994,19(5):609～618[Feng Qinglai. On outcrop sequence stratigraphy of intraplatform trough and sea level change during early Carboniferous in northwestern Guangxi[J]. Earth Science, 1994,19(5):609～618]
[3]	侯中健,陈洪德,田景春.右江盆地海相泥盆系-中三叠统层序界面成因类型与盆地演化[J].沉积学报,2000,18(2):205～209[Hou Zhongjian,Chen Hongde,Tian Jingchun,et al. Genesis of sequence boundary and basin evolution in Youjiang basin during the Devonian to the Middle Triassic[J]. Acta Sedimentologica Sinica, 2000,17(4):205～209]
[4]	贾振远,蔡华,蔡忠贤.中国古大陆及其边缘早古生代层序地层及海平面变化的基本特征[J].地球科学,1997,22(5):544～551[Jia Zhenyuan,Cai Hua, Cai Zhongxian. Sequence stratigraphy and sea level change of the Ordovician in the southern margin of Ordos region[J]. Earth Science, 1997,22(5):544～551]
[5]	李儒峰,刘本培,赵澄林.扬子板块石炭纪沉积层序及全球性对比研究[J].沉积学报,1997,15(3):23～28[Li Rufeng, Liu Benpei, Zhao Chenglin. Correlation of Carboniferous depositional sequences on the Yangtze plate with others on a global scale[J]. Acta Sedimentologica Sinica, 1997,15(3);23～28]
[6]	彭军,陈洪德,田景春,等.川黔桂地区石炭系层序地层学研究[J].沉积学报,2000,18(2):190～197[Peng Jun,Chen Hongde,Tian Jingchun, et al. Sequence stratigraphy study on the Caboniferous strata in Sichuan,Yunnan,Guizhou and Guangxi[J]. Acta Sedimentologica Sinica, 2000,17(4): 190～197]
[7]	覃建雄,陈洪德,田景春,等.川滇黔桂地区泥盆系层序地层分析[J].沉积学报,2001,18(2):172～180[Qin Jianxiong, Chen Hongde, Tian Jingchun, et al. Sequence stratigraphy of Devonian in the Youjiang basin[J]. Acta Sedimentologica Sinica,2000,17(4):172～179]
[8]	田景春,陈洪德,彭军,等.右江盆地深水沉积层序地层学研究[J].沉积学报,2000,18(2):210～214[Tian Jingchun,Chen Hongde,Peng Jun, et al. Study on sequence stratigraphy of deep water sediments in Youjiang basin[J]. Acta Sedimentologica Sinica, 2000,17(4):210～214]
[9]	吴诒,龚一鸣,李德清.华南泥盆系层序地层与岩石、年代地层界线间相关性探讨[J].地球科学,1994,19(5):565～574[Wu Yi, Gong Yiming, et al. Correlation of sequence stratigraphy to lithostratigraphy and chronostratigraphy of Devonian in South China[J].Earth Science, 1994,19(5):565～574]
[10]	徐世球. 川黔湘交境寒武纪二级层序的划分及海平面变化[J].地球科学,1997a,22(5):467～470[Xu Shiqiu.The secong-order sequence division and sea level fluctuation in Cambrian on the border of Sichuan,Guizhou and Hunan[J]. Earth Science, 1997a, 22(5):467～470]
[11]	Brett C E, Goodman W M, LoDuca S P. Sequence stratigraphy and basin dynamics in the Silurian of Appalachian foreland basin[J]. Sedimentary Geology, 1990, 69(3/4):191～224
[12]	Galloway W E. Genetic stratigraphic sequences in basin analysis[J]. AAPG Bulletin, 1989,73:125～154
[13]	Hallam A. Pre-Quaternary changes of sea level[J]. Annual Review Planet Earth Science, 1984,12:205～243
[14]	Miall A D. Stratigraphic sequences and their chronostratigraphic correlation[J]. Journal of Sedimentary Petrology, 1992,61(4): 497～505
[15]	Pitman W C. Relationship between eustacy and stratigraphic sequences of passive margins[J]. Geology Sociaty of America Bulletin, 1978,89:1 389～1 403
[16]	Ross C A, Ross J R P. Late Paleozoic sea levels and depositional sequences[A]. In: Ross C A, Haman D, eds. Timing and Depositional History of Eustatic Sequences:Constraints on Seismic Stratigraphy[C]. Cushman Found Foram Res, Spec Publ, 1987,24:137～149
[17]	Vail P R, Hardenbol J. Sea-level changes during the Tertiary[J]. Oceans, 1979,22:71～79
[18]	Van Wagoner J C, Betram G T. Sequence stratigraphy of foreland basin deposits[J]. AAPG Memoir, 1995,64:1～487
[19]	Weimer P, Posamentier H W. Siliciclastic sequence stratigraphy recent developments and applications[J].AAPG Memoir, 1994,58:1～492
[20]	Wilgus C K, Hastings B S, Kendall C G St C, et al.Sea level changes: an integrated approach[J]. SEPM Special Publishing, 1988,42:1～407

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The Apparent Types of Sequence Bottom Boundary Surface--Taking marine Sinian System to Middle Triassic Series in South China as an example

State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation Institute of Sedimentology, Chengdu University of Technology, Chengdu 610059

Received Date: 2002-05-31

Rev Recd Date: 2002-09-09

Publish Date: 2003-12-10

Key words:

Abstract: It is well known that the key of research on sequence stratigraphy is sequence division, but first of all the key of sequence division is identification of boundary surface. The boundary surface of defined sequence included sequence bottom boundary surface first trangressive surface and maximum marine f looding surface. Among them, the most important is bottom boundary surface indentification because it is sequence division foundation. The paper, taking marine Sinian system to Middle Triassic Series in south China as an example, through anlyses of filed geologic sections, identified nine types sequence bottom boundary surfaces which are: ( 1) weathering crust;(2) Paleosol;(3) Erosion surface of river rejuvenation;(4) Action surface of ancient karst;(5) Washing erosion surface of gravity flow on slop;(6) Erosion surface of turbidity flow in basin;(7) Action surface of volcano event;(8) Transition surface of rock character and facies;(9) onlap surface. Research features of above boundary surfaces in detail is very important for sequence division.

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Reference (20)

[1]	陈洪德,覃建雄,田景春,等.右江盆地层序充填动力学初探[J].沉积学报,2000,18(2):165～171[Chen Hongde,Qin Jianxiong,Tian Jingchun,et al. Sequence filling dynamics of Youjiang basin,Southern China[J]. Acta Sedimentologica Sinica, 2000,17(4):165～171]
[2]	冯庆来.桂西北早石炭世台槽地区露头层序地层及海平面变化研究[J].地球科学,1994,19(5):609～618[Feng Qinglai. On outcrop sequence stratigraphy of intraplatform trough and sea level change during early Carboniferous in northwestern Guangxi[J]. Earth Science, 1994,19(5):609～618]
[3]	侯中健,陈洪德,田景春.右江盆地海相泥盆系-中三叠统层序界面成因类型与盆地演化[J].沉积学报,2000,18(2):205～209[Hou Zhongjian,Chen Hongde,Tian Jingchun,et al. Genesis of sequence boundary and basin evolution in Youjiang basin during the Devonian to the Middle Triassic[J]. Acta Sedimentologica Sinica, 2000,17(4):205～209]
[4]	贾振远,蔡华,蔡忠贤.中国古大陆及其边缘早古生代层序地层及海平面变化的基本特征[J].地球科学,1997,22(5):544～551[Jia Zhenyuan,Cai Hua, Cai Zhongxian. Sequence stratigraphy and sea level change of the Ordovician in the southern margin of Ordos region[J]. Earth Science, 1997,22(5):544～551]
[5]	李儒峰,刘本培,赵澄林.扬子板块石炭纪沉积层序及全球性对比研究[J].沉积学报,1997,15(3):23～28[Li Rufeng, Liu Benpei, Zhao Chenglin. Correlation of Carboniferous depositional sequences on the Yangtze plate with others on a global scale[J]. Acta Sedimentologica Sinica, 1997,15(3);23～28]
[6]	彭军,陈洪德,田景春,等.川黔桂地区石炭系层序地层学研究[J].沉积学报,2000,18(2):190～197[Peng Jun,Chen Hongde,Tian Jingchun, et al. Sequence stratigraphy study on the Caboniferous strata in Sichuan,Yunnan,Guizhou and Guangxi[J]. Acta Sedimentologica Sinica, 2000,17(4): 190～197]
[7]	覃建雄,陈洪德,田景春,等.川滇黔桂地区泥盆系层序地层分析[J].沉积学报,2001,18(2):172～180[Qin Jianxiong, Chen Hongde, Tian Jingchun, et al. Sequence stratigraphy of Devonian in the Youjiang basin[J]. Acta Sedimentologica Sinica,2000,17(4):172～179]
[8]	田景春,陈洪德,彭军,等.右江盆地深水沉积层序地层学研究[J].沉积学报,2000,18(2):210～214[Tian Jingchun,Chen Hongde,Peng Jun, et al. Study on sequence stratigraphy of deep water sediments in Youjiang basin[J]. Acta Sedimentologica Sinica, 2000,17(4):210～214]
[9]	吴诒,龚一鸣,李德清.华南泥盆系层序地层与岩石、年代地层界线间相关性探讨[J].地球科学,1994,19(5):565～574[Wu Yi, Gong Yiming, et al. Correlation of sequence stratigraphy to lithostratigraphy and chronostratigraphy of Devonian in South China[J].Earth Science, 1994,19(5):565～574]
[10]	徐世球. 川黔湘交境寒武纪二级层序的划分及海平面变化[J].地球科学,1997a,22(5):467～470[Xu Shiqiu.The secong-order sequence division and sea level fluctuation in Cambrian on the border of Sichuan,Guizhou and Hunan[J]. Earth Science, 1997a, 22(5):467～470]
[11]	Brett C E, Goodman W M, LoDuca S P. Sequence stratigraphy and basin dynamics in the Silurian of Appalachian foreland basin[J]. Sedimentary Geology, 1990, 69(3/4):191～224
[12]	Galloway W E. Genetic stratigraphic sequences in basin analysis[J]. AAPG Bulletin, 1989,73:125～154
[13]	Hallam A. Pre-Quaternary changes of sea level[J]. Annual Review Planet Earth Science, 1984,12:205～243
[14]	Miall A D. Stratigraphic sequences and their chronostratigraphic correlation[J]. Journal of Sedimentary Petrology, 1992,61(4): 497～505
[15]	Pitman W C. Relationship between eustacy and stratigraphic sequences of passive margins[J]. Geology Sociaty of America Bulletin, 1978,89:1 389～1 403
[16]	Ross C A, Ross J R P. Late Paleozoic sea levels and depositional sequences[A]. In: Ross C A, Haman D, eds. Timing and Depositional History of Eustatic Sequences:Constraints on Seismic Stratigraphy[C]. Cushman Found Foram Res, Spec Publ, 1987,24:137～149
[17]	Vail P R, Hardenbol J. Sea-level changes during the Tertiary[J]. Oceans, 1979,22:71～79
[18]	Van Wagoner J C, Betram G T. Sequence stratigraphy of foreland basin deposits[J]. AAPG Memoir, 1995,64:1～487
[19]	Weimer P, Posamentier H W. Siliciclastic sequence stratigraphy recent developments and applications[J].AAPG Memoir, 1994,58:1～492
[20]	Wilgus C K, Hastings B S, Kendall C G St C, et al.Sea level changes: an integrated approach[J]. SEPM Special Publishing, 1988,42:1～407

The Apparent Types of Sequence Bottom Boundary Surface--Taking marine Sinian System to Middle Triassic Series in South China as an example

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