塔中地区中晚奥陶世内波、内潮汐沉积

高振中; 何幼斌; 张兴阳; 翟永红; 胡云扬; 杨海军; 李新生; 李勇

塔中地区中晚奥陶世内波、内潮汐沉积

1 江汉石油学院地质系湖北荆州 434102;
2 塔里木石油勘探开发指挥部勘探研究中心新疆库尔勒 841000

基金项目: 国家自然科学基金资助项目(批准号:49872050)的研究成果之一

详细信息

作者简介:
高振中,男,1937年出生,教授,沉积学与石油地质学

中图分类号: P512.2

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Internal－ Wave and Internal－ Tide Deposits of the Middle－ Upper Ordovician in the Center Tarim Basin

1 Department of Geology, Jianghan Petroleum Institute, Jingzhou, Hubei 434102;
2 Tarim Petroleum Exploration and Development Headquarter, Korla, Xinjiang 841000

摘要

摘要: 现代海底普遍发育由内波、内潮汐引起的深水牵引流,内波、内潮汐不仅可形成各种厘米级的深水牵引流沉积构造,还可建造千米级的大型沉积物波。这种大型沉积物波既可沿斜坡向下迁移,也可沿斜坡向上迁移。在古代地层记录中已发现各种厘米级的内波、内潮汐沉积单元,但尚未发现内波成因的大型沉积物波。塔中地区中上奥陶统碎屑岩段内发育内波及内潮汐形成的各种牵引流沉积构造单元。通过详细的岩心观察,识别出 4种内波、内潮汐沉积微相类型及 5种基本垂向沉积层序。此外,通过地震剖面分析,在研究区中上奥陶统陆坡相中识别出顺坡向上迁移的大型沉积物波,该沉积物波的特征与现代海底发育的沉积物波的特征类似,运用内波理论可对其成因进行合理的解释。
- 深水牵引流沉积 /
- 内波 /
- 内潮汐 /
- 大型沉积物波 /
- 沉积微相 /
- 沉积层序 /
- 沉积模式
Abstract: Deep一water traction currents of internal一wave and internal一ride origin are well developed on modern sea floor. They can not only produce sedimentary structures of cm一size but also build large一sca1e sediment waves of km一size. Moreover, mast of these sediment waves migrate upslope. In ancient stratigraphic record, small一scale sedimentation units of internal一wave and internal一tide origin have been recognized Gut large一scale sediment waves of internal一wave origin have not. Based on detailed studies, different kinds of internal一wave and internal 一tide deposits have been recognized in the clastic rocks of the middle一upper Ordovician in the Central Tarim Basin. Four basiC sedimentary micrpfacies and five identical successions of internal一wave and internal一tide de- posits have been recognized and summarized. These microfacies are (1)hi一directional cross一laminated very fine- grained sandstone microfacies, (2)unidirectional cross一bedded and bi一directional crass一laminated medium一to fine一grained sandstone microfacies, (3)alternating sandstone and mudstone microfacies, and (4)oolitic limestone andsand politic limestone microfacies. The vertical successions include (l)symmetrical graded succession consisting entirely of cross一laminated sandstone, (2)normal graded succession consisting of cross一laminated sandstone, (3) normal graded succession consisting of medium scale cross一bedding and bi一directional cross一laminations, (4) symmetrical graded一couplet succession, (5)mudstone一oolitic limestone一mudstone succession. More importantly, based on detailed studies of seismic profiles, the authors discovered large一scale sediment waves of upslope migra- tion developed in the continental slope facies of the middle一upper Ordovician. The characteristics of these sedi- meat waves are similar to those of the sediment waves well developed on modem seafloor. According to the theory of internal wave, the origin of these sediment waves can be explained satisfactorily.
- deep一water traction current deposits /
- internal wave /
- internal tide /
- sediment waves /
- sedimentary facies /
- vertical succession /
- sedimentation model

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参考文献(21)

[1]	LaFond E C. Internal Waves[A] . In: Feirbridge G W,ed. The ency-clopedia of oceanography[C] . New York: Reinhold, 1966. 402～408
[2]	Shepard F P, Marshall N F, McLoughlin P A, Sullivan G G. Currentsin submarine canyons and other sea valleys[M] : American Associationof Petroleum Geologists Studies in Geology 8, 1979. 173
[3]	Munk W. Internal waves and small - scale processes[A] . In: Warren BA, Wunsch C, eds. Evolution of physical oceanography [C] . Cam-bridge, Massachtsetts Institute of Technology, 1981. 264～191
[4]	Gao Zhenzhong, Eri ksson K A. Internal - tide deposits in an Ordovi-cian submarine channel: Previously unrecognized facies? [J] . Geology,1991, 19(7): 734～737
[5]	高振中,Eriksson K A.美国阿巴拉契亚山脉芬卡苏地区奥陶纪海底水道中的内潮汐沉积[J] .沉积学报,1993,11(1)：12～22
[6]	高振中,何幼斌,罗顺社,郭建华.深水牵引流沉积－内潮汐、内波和等深流沉积研究[M] .北京：科学出版社,1996
[7]	高振中,何幼斌,李建明,李维峰,罗顺社,王泽中.我国发现内潮汐沉积[J] .科学通报,1997,42(13)：1418～1421
[8]	高振中,彭德堂,刘学锋,何幼斌,符翔,李东升,钟广法.塔里木盆地1Z30井中奥陶统内潮汐沉积[J] .江汉石油学院学报,1996,18(4)：9～14
[9]	Howe J A. Turbidite and contourite sediment waves in the northernRockall Trough, North Atlantic Oeean[J ] . Sedimentology, 1996, 43:219～234
[10]	Richard P C, Ritchie J D, Thomson A R. Evolution of deep - waterclimbing dunes in the Rokall Trough - - implications for overflow cur-rents across the Wyville- Thomson Ridge in the Late Miocene[J] .Marine Geology, 1987, 76:177～183
[11]	Damuth J E. Migrating sediment waves created by turbidity currentsin the northern south China sea[J] . Geology, 1979, 7:520～523
[12]	NorrnarkWR, HessGR, StowDAV, BowenAJ. Sediment waveson the monterey fanlevee: a preliminary physical interpretation[J ] .Marine Geology, 1980, 37:1～18
[13]	Flood R D, Sbor A N. Mud waves in the Argentine basin and their re-lationship to regional bottom circulation patterns[J] . Deep - sea Res.,1988, 35:943～971
[14]	Gao Zhenzhong, Eriksson K A, He Youbin, et al. Deep- WaterTraction Current Depcsits－A Study of Internal Tides, InternalWaves, Contour Currents and Their Deposits[ M ] . Beijing and NewYork: Science Press, Utrecht and Tokyo: VSP, 1998
[15]	Karl H A. Internal - wave currents as a mechanism to account forlarge sand waves in Navarinsky Canyon Head, Bering Sea[J ] . J. Sed-ment. Petrol., 1986, 56(5): 706～714
[16]	张兴阳,高振中,姚雪根.北大西洋洛克尔海槽东北部内波沉积[J] .沉积学报,1999,17(3)：464～472
[17]	何幼斌,罗顺社,高振中.深水牵引流沉积研究进展与展望[J] .地球科学进展,1997,12(3)：247～252
[18]	何幼斌,高振中.内潮汐、内波沉积的特征与鉴别[J] .科学通报,1998, 43(9): 903～908
[19]	Shanmngam G, Spalding T D, Rofheart D H. Process sedimentologyand reservoir quality of deep- marine bottom - current reworked sands(sandy contourites): an example from the Gulf of Mexico[J] . AAPGBulletin,1993,77：1241～1259
[20]	杨殿荣.海洋学[M] .北京：高等教育出版社,1985
[21]	LaFond E C. Internal waves[A] . In: Hill M N, ed. The sea[C] Volume 1. London: Wiley Interscience, 1962. 731～751

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塔中地区中晚奥陶世内波、内潮汐沉积

作者简介:
高振中,男,1937年出生,教授,沉积学与石油地质学

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Internal－ Wave and Internal－ Tide Deposits of the Middle－ Upper Ordovician in the Center Tarim Basin

计量

目录

塔中地区中晚奥陶世内波、内潮汐沉积

1 江汉石油学院地质系湖北荆州 434102;

2 塔里木石油勘探开发指挥部勘探研究中心新疆库尔勒 841000

作者简介:
高振中,男,1937年出生,教授,沉积学与石油地质学

English Abstract

Internal－ Wave and Internal－ Tide Deposits of the Middle－ Upper Ordovician in the Center Tarim Basin

1 Department of Geology, Jianghan Petroleum Institute, Jingzhou, Hubei 434102;

2 Tarim Petroleum Exploration and Development Headquarter, Korla, Xinjiang 841000

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塔中地区中晚奥陶世内波、内潮汐沉积

作者简介: 高振中,男,1937年出生,教授,沉积学与石油地质学

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出版历程

Internal－ Wave and Internal－ Tide Deposits of the Middle－ Upper Ordovician in the Center Tarim Basin

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出版历程

目录

塔中地区中晚奥陶世内波、内潮汐沉积

1 江汉石油学院地质系 湖北荆州 434102; 2 塔里木石油勘探开发指挥部勘探研究中心 新疆库尔勒 841000

作者简介: 高振中,男,1937年出生,教授,沉积学与石油地质学

English Abstract

Internal－ Wave and Internal－ Tide Deposits of the Middle－ Upper Ordovician in the Center Tarim Basin

1 Department of Geology, Jianghan Petroleum Institute, Jingzhou, Hubei 434102; 2 Tarim Petroleum Exploration and Development Headquarter, Korla, Xinjiang 841000

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
高振中,男,1937年出生,教授,沉积学与石油地质学

1 江汉石油学院地质系湖北荆州 434102;

2 塔里木石油勘探开发指挥部勘探研究中心新疆库尔勒 841000

作者简介:
高振中,男,1937年出生,教授,沉积学与石油地质学

1 Department of Geology, Jianghan Petroleum Institute, Jingzhou, Hubei 434102;

2 Tarim Petroleum Exploration and Development Headquarter, Korla, Xinjiang 841000