OCCURRING OF THE EAST CHINA YANSHANIAN PLATEAU AND ITS INSPIRATION TO MINERAL AND PETROLEUM RESOURCES EVALUATION

WU Gen-yao; CHEN Huan-jiang; MA Li; XU Ke-ding

doi:10.11781/sysydz200201003

Volume 24 Issue 1

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WU Gen-yao, CHEN Huan-jiang, MA Li, XU Ke-ding. OCCURRING OF THE EAST CHINA YANSHANIAN PLATEAU AND ITS INSPIRATION TO MINERAL AND PETROLEUM RESOURCES EVALUATION[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2002, 24(1): 3-12. doi: 10.11781/sysydz200201003

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WU Gen-yao, CHEN Huan-jiang, MA Li, XU Ke-ding. OCCURRING OF THE EAST CHINA YANSHANIAN PLATEAU AND ITS INSPIRATION TO MINERAL AND PETROLEUM RESOURCES EVALUATION[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2002, 24(1): 3-12. doi: 10.11781/sysydz200201003

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OCCURRING OF THE EAST CHINA YANSHANIAN PLATEAU AND ITS INSPIRATION TO MINERAL AND PETROLEUM RESOURCES EVALUATION

doi: 10.11781/sysydz200201003

1.
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
2. Department of Marine Geology & Geophysics, Tongji University, Shanghai 200092, China
3. Jiangsu oil field, SINOPEC, Jiangdu, Jiangsu 225261, China
4. Zhejiang Division of Petroleum Exploration, CNPC, Hangzhou, Zhejiang 310013, China

Received Date: 2001-11-08
Publish Date: 2002-01-25

Abstract

Abstract

It is first represented that the Su-Wan(Jiangsu-Anhui)Block is an independent tectonic unit in the period of Tethyan evolution.Based on the research fruits of igneous rocks,metamorphic rocks and paleogeomagnetism,it is thought that the Su-Lu(Jiangsu-Shandong)Ocean closed in the Late Jurassic-Early Cretaceous at last,the collision of the Su-Wan Block with the North China Craton resulted in the appearance of the plateau,and the East China Yanshanian Plateau should belong to collision plateaus in its features.In this paper,the thrust-nappe zone on the margin of the plateau and its internal complex structure,including relative high and steep spaces developing along major collision-shear zones and relative open intermountain molasse basins,are also discussed.It is considered that the plateau is a part of the grand scale East Asia Yanshanian Orogenic Series with relative weak deformation and metamorphism.The plateau had collapsed since the end of the Early Cretaceous.The Late Cretaceous was the overall collapsing period of the East Asia Yanshanian Orogenic Series.In the Tertiary,the Yanshanian plateau did not exist at all.Strong magmatic activities made Yanshanian mineralization possess obvious regional specialization not only in Su-Wan area but also in Jiaodong,Xiaoqinling and Northeast Jiangxi areas.The Late Mesozoic-Cenozoic tectonic events resulted in the low strength lithosphere and high geothermal gradient in Su-Wan to the Huanghai Sea area.On this basis,the petroleum prospects are evaluated.

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References(54)

References

[1]	Liou J G,Zhang R Y,Wang X,et al.Metamorphism and tectonics of HP and UHP belts in the Dabie-Sulu region,China[A].Yin A and Harrison T M. Tectonic Evolution of Asia[M].Cambridge: Cambridge Univ Press,1995.345-370.
[2]	杨文采.胡振远.程振炎,等.郯城-涟水综合地球物理剖面[J].地球物理学报,1999,42(2):206-217.
[3]	Zhang G W,Xiang L W,Meng Q R.The Qinling orogen and intracontinental orogen mechanisms[J].Episodes,1995,18(1-2):36-39.
[4]	朱炳泉.地球化学急变带及对中国南方油气勘探的思考[J].海相油气地质,1997,2(4):1-3.
[5]	樊金涛.苏北东海晋宁期蛇绿岩与苏胶造山带演化[J].江苏地质,1996,20(1):1-8.
[6]	樊金涛.苏北蛇绿岩[J].桂林工学院学报,1998,18(2):136-144.
[7]	潘明宝.江苏大地构造研究与展望[J].江苏地质,1998,22(增刊):12-16.
[8]	Wu Genyao,Yano T and Inomata M.Yanshanian orogenics in South China:a relation to Neotethyan evolution[J].Scientia Geologica Sinica,1998,7(1):1-10.
[9]	邵济安.唐克东,等.中国东北地体与东北亚大陆边缘演化[M].北京:地震出版社,1995.1-185.
[10]	Zorin Y A,Belicchenko V G,Turutanov E K,et al.The East Siberia Transect[J].International Geol Review,1995,37:154-175.
[11]	Hada S,Ishii K,Landis C A,et al.Kurosegawa terrane in southwest Japan:disrupted remnants of a Gondwana-derived terrane[J].Gondwana Research,2001,4(1):27-38.
[12]	邓晋福,叶德隆,赵海玲,等.下扬子地区火山作用深部过程与盆地形成[M].武汉:中国地质大学出版社,1992,1-183.
[13]	邓晋福,赵国春,赵海玲,等.中国东部燕山期火成岩构造组合与造山-深部过程[J].地质论评,2000,46(1):41-48.
[14]	江苏省地质矿产局.江苏省及上海市区域地质志[M].北京:地质出版社,1984.1-857.
[15]	任启江,刘若善,徐兆文,等.安徽庐枞中生代火山构造洼地及其成矿作用[M].北京:地质出版社,1991.1-206.
[16]	翟裕生,姚书振,林新多,等.长江中下游地区铁铜(金)成矿规律[M].北京:地质出版社,1992.1-235.
[17]	常印佛,刘湘培,吴言昌.长江中下游铜铁成矿带[M].北京:地质出版社,1991.1-379.
[18]	倪若水,吴其切,岳文浙,等.长江中下游中生代陆相盆地演化与成矿作用[M].上海:科学技术文献出版社,1998.1-118.
[19]	张旗,钱青,王二七,等.燕山中晚期的中国东部高原:埃达克岩的启示[J],地质科学,2001,36(2):248-255.
[20]	周王旬若,任进.长江中下游中生代花岗岩[M].北京:地质出版社,1994.1-119.
[21]	徐安中.苏北云台群含蓝晶石岩石矿物组合特征及其地质意义[J].江苏地质,1998,22(1):10-14.
[22]	张永鸿.地星演化(球面构造地质学立论基础)[M].南京:南京大学出版社,1996.1-552.
[23]	钟大赉,等.滇川西部古特提斯造山带[M].北京:科学出版社,1998.1-231.
[24]	裴先治,李厚民,李国光,等.东秦岭商丹构造带主要地质体的同位素年龄及其构造意义[J].地球学报,1997,18(增刊):40-42.
[25]	吴汉宁,常承法,刘椿,等.依据古地磁资料探讨华北和华南块体运动及其对秦岭造山带构造演化的影响[J].地质科学,1990,(3):201-214.
[26]	安徽省地质矿产局.安徽省区域地质志[M].北京:地质出版社,1987.1-721.
[27]	赵宗举,杨树锋,陈汉林,等.河南商城-固始地区石炭系沉积环境及其构造意义[J].地质论评,2000,46(4):407-416.
[28]	和政军,李锦轶,牛宝贵,等.燕山-阴山地区晚侏罗世强烈推覆-隆升事件及沉积响应[J].地质论评,1998,44(4):407-418.
[29]	张抗.鄂尔多斯断块构造和资源[M].西安:陕西科学技术出版社,1989.1-394.
[30]	吴根耀.古深断裂活化与燕山期陆内造山运动——以川南-滇东和中扬子褶皱-冲断系为例[J].大地构造与成矿学,2001,25(3):246-253.
[31]	河南省地质矿产局.河南省区域地质志[M].北京:地质出版社,1989.1-772.
[32]	Wu Genyao.Rejuvenation of fossil sutures and related Mesozoic intracontinental orogenies in South China[J].Acta Geologica Sinica (English edition),2000,74(2):194-200.
[33]	Hayama Y,Inomata M,Koido Y,et al.Comparative geological study between Fujian region in China and Inner Zone of southeast Japan[J].Scientia Geologica Sinica,1996,5(4):425-434.
[34]	吴根耀.华南的格林威尔造山带及其坍塌在罗迪尼亚超大陆演化中的意义[J].大地构造与成矿学,2000,24(2):112-123.
[35]	Wu G Y.Tethyan evolution in South China and its environs[A].Xiao Xuchang and Liu Hefu.Global Tectonic Zones,Supercontinent Formation and Disposal[M].Utrecht:VSP,1997.55-76.
[36]	Wu G Y.Main tectonic units and geological evolution in South China and its environs: in the light of Gondwana dispersion and Asian accretion[A].Metcalfe I.Gondwana Dispersion and Asian Accretion[M].Rotterdam: A A Balkema,1999.315-340.
[37]	朱光,王道轩,刘国生,等.郯庐断裂带的伸展活动及其动力学背景[J].地质科学,2001,36(3):269-278.
[38]	铃木和博,端山好和,猪俣道也,吴根耀.福建石狮白垩纪片麻状花岗岩的CHIME年龄[J].科学通报,1997,42(12):1 343-1 344.
[39]	岳文浙,业治铮,魏乃颐,等.长江中下游威宁期沉积地质与块状硫化物矿床[M].北京:地质出版社,1993.1-163.
[40]	康永成,吴言昌,储国正,等.安徽沿江地区铜-多金属矿床地质[M].北京:地质出版社,1998.1-351.
[41]	邓军,杨立强,刘伟,等.胶东招掖矿集区巨量金质来源和流体成矿效应[J].地质科学,2001,36(3):257-268.
[42]	周伟新,万天丰.玲珑花岗岩体的变形磁组构特征及其与金矿关系[J].地质科学,2000,35(4):385-395.
[43]	河南省地质矿产局.太峪口、巴楼和岳渡幅区域地质图(1∶50 000)[M].北京:地质出版社,1993.
[44]	张进江,郑亚东,刘树文.小秦岭金矿中生代构造演化与矿床形成[J].地质科学,2002,(待刊).
[45]	朱训,黄崇轲,芮宗瑶,等.德兴斑岩铜矿[M].北京:地质出版社,1983.1-336.
[46]	华仁民,李晓峰,陆建军,等.德兴大型铜金矿集区构造环境和成矿流体研究进展[J].地球科学进展,2000,15(5):525-533.
[47]	俞凯,郭念发.下扬子区下古生界油气地质条件评价[J].石油实验地质,2001,23(1):41-46.
[48]	李成,王良书,杨春.下扬子区岩石圈双层脆韧性过渡带叠置的流变学证据[J].地质论评,2001,47(3): 245-249.
[49]	Klemme H D and Ulmishek G F.Effective petroleum source rocks of the world: stratigraphic distribution and controlling depositional factors[J].AAPG Bull,1991,75:1 809-1 851.
[50]	孙肇才,邱蕴玉,郭正吾.板内形变与晚期次生成藏——扬子区海相油气总体形成规律的探讨[J].石油实验地质,1991,13(2):107-142.
[51]	赵文智,窦立荣,宋岩.我国天然气地质研究和勘探的新进展[J].天然气工业,2000,20(3):1-6.
[52]	邓晋福,莫宣学,赵海玲,等.中国东部岩石圈根/去根作用与大陆活化[J].现代地质,1994,8(3):349-356.
[53]	邓晋福,赵海玲,莫宣学,等.中国大陆根-柱构造——大陆动力学的钥匙[M].北京:地质出版社,1996.1-110.
[54]	董树文,吴锡浩,吴珍汉,等.论东亚大陆的构造翘变——燕山运动的全球意义[J].地质论评,2000,46(1):7-13.

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OCCURRING OF THE EAST CHINA YANSHANIAN PLATEAU AND ITS INSPIRATION TO MINERAL AND PETROLEUM RESOURCES EVALUATION

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OCCURRING OF THE EAST CHINA YANSHANIAN PLATEAU AND ITS INSPIRATION TO MINERAL AND PETROLEUM RESOURCES EVALUATION

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