Advanced Search
Volume 25 Issue 6
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2003  >  25(6): 670-678
ZHAO Zong-ju, ZHU Yan, XU Chun-hua, ZHOU Jin-gao, YI Wan-xia, SHEN Jin-long. COUPLING RELATIONS BETWEEN THE HEFEI BASIN AND THE DABIE-ZHANGBALING OROGENIC BELT[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2003, 25(6): 670-678. doi: 10.11781/sysydz200306670
Citation: ZHAO Zong-ju, ZHU Yan, XU Chun-hua, ZHOU Jin-gao, YI Wan-xia, SHEN Jin-long. COUPLING RELATIONS BETWEEN THE HEFEI BASIN AND THE DABIE-ZHANGBALING OROGENIC BELT[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2003, 25(6): 670-678. doi: 10.11781/sysydz200306670
shu

COUPLING RELATIONS BETWEEN THE HEFEI BASIN AND THE DABIE-ZHANGBALING OROGENIC BELT

doi: 10.11781/sysydz200306670
  • 1.

    Hangzhou Research Institute of Geology, CNPC, Hangzhou, Zhejiang 310023, China

  • 2. Department of Earth Sciences, Zhejiang University, Hangzhou, Zhejiang 310027, China

  • 3. Shengli Oilfield, SINOPEC, Dongying, Shandong 257015, China

  • Received Date: 2003-06-07
  • Rev Recd Date: 2003-10-15
  • Publish Date: 2003-11-25
    Abstract
  • The existing Dabie-Zhangbaling Orogenic Belt,whose formation and evolution apparently controlled the features and evolution of the Meso-Cenozoic Hefei Basin,has been formed since the Indosinian epoch.There were close coupling relations between the basin types and its reforming styles of the Hefei Basin in the different periods of the Meso-Cenozoic and the moving styles of the Dabie-Zhangbaling Orogenic Belt:a) the coupling of the thrust reformation in the Indosinian (the Middle-Late Triassic) displayed in where the Hefei Basin is with the syncollision compressive obduction orogenesis which resulted in the final collision and matching of the Yangtze Plate and the Huabei Plate and the formation of the Dabie-Zhangbaling Orogenic Belt;b) the coupling of the formation of the paraforeland Hefei Basin in the Jurassic with the strong buoyancy diapir orogenic uplifting of the Dabie-Zhangbaling Orogenic Balt resulted from the folding subsidence of the underthrust Yangtze Plate and the further matching compressive orogenesis of the Yangtze-Huabei Landmass;c) the coupling of the formation of the slide-overlap and strike-slip composite Hefei Basin in the Early Cretaceous with the thermal-uplifting extension of the Dabie Orogenic Belt and the strike-slip movement of the Zhangbaling Orogenic Belt;d) the coupling of the thrust reformation displayed by the major Hefei Basin in the early stage of the Late Cretaceous and the formation of down-warped basins in the northeast part with the thermal-uplifting extension of the Dabie Orogenic Belt and the weak compression of the Zhangbaling Orogenic Belt;e) the coupling of the formation of tenso-shear rift basins in the late stage of the Late Cretaceous to the Paleogene with the postorogenic collapse of the Dabie-Zhangbaling Orogenic Belt and the differential elevation and subsidence of fault blocks;f) the Dabie-Zhangbaling Orogenic Belt since the main episode of the Himalayan movement in the Oligocene totally displaying weakly compressive and compresso-shear orogenic uplifting and being gradually denuded and leveled,and providing material sources for the down-warped deposition of the Hefei Basin in the Neogene-Quaternary.

     

    • FullText(HTML)
  • loading
    • References(53)
  • [1]
    王清晨,从柏林,马力.大别山造山带与合肥盆地的构造耦合[J].科学通报,1997,42(6):575－580.
    [2]
    宋明水,江来利,李学田,等.大别山造山带对合肥盆地的构造控制[J].石油实验地质,2002,24(3):209－215.
    [3]
    李忠,孙枢,李任伟,等.合肥盆地中生代充填序列及其对大别山作用的指示[J].中国科学(D辑 地球科学),2000,30(3):256－263.
    [4]
    王道轩,刘因,李双应,等.大别超高压变质岩折返至地表的时间下限:大别山北麓晚侏罗世砾岩中发现榴辉岩砾石[J].科学通报,2001,46(14):1216－1220.
    [5]
    刘少峰,张国伟,张宗清,等.合肥盆地花岗岩砾石的同位素年代学示踪[J].科学通报,2001,46(9):748－753.
    [6]
    李双应,岳书仓,王道轩,等.大别造山带超高压变质岩折返隆升的地层学证据——毛坦厂组榴辉岩砾岩的启示[J].地质论评,2002,48(4):345－352.
    [7]
    刘国生,朱光,王道轩,等.郯庐断裂带张八岭隆起段走滑运动与合肥盆地的沉积响应[J].沉积学报,2002,20(2):267－273.
    [8]
    朱光,牛漫兰,刘国生,等.郯庐断裂带早白垩世走滑运动中的构造、岩浆、沉积事件[J].地质学报,2002,76(3):325－334.
    [9]
    翟明国,从柏林.苏鲁-大别山变质带岩石大地构造学[J].中国科学(D辑 地球科学),1996,26(3):258－264.
    [10]
    董树文,孙先如,张勇,等.大别山碰撞造山带基本结构[J].科学通报,1993,38(6):542－545.
    [11]
    李曙光,Hart-S-R,郑双根,等.中国华北、华南陆块碰撞时代的钐－铷同位素年龄证据[J].中国科学(B辑),1989,(3):312－319.
    [12]
    刘若新,樊祺诚,李惠民,等.大别山碧溪岭石榴石橄榄岩－榴辉岩高压变质作用的年代学研究[J].科学通报,1995,40(14):1304－1306.
    [13]
    刘育燕,杨巍然,森永速男,等.华北、秦岭及扬子陆块的若干古地磁研究结果[J].地球科学——中国地质大学学报,1993,18(5):635－641.
    [14]
    赖旭龙,殷鸿福,杨逢清.秦岭三叠纪古海洋再造[J].地球科学——中国地质大学学报,1995,20(6):648-656.
    [15]
    董树文,方景爽,李勇,等.下扬子中三叠世-中侏罗世沉积相与印支运动[J].地质论评,1994,40(2):111－119.
    [16]
    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.
    [17]
    夏文臣,周杰,袁伟,等.华南晚三叠世前陆盆地的成因地层格架及演化历史[J].地球科学——中国地质大学学报,1994,19(1):19－29.
    [18]
    朱光,徐嘉炜,刘国生,等.下扬子地区前陆变形构造格局及其动力学机制[J].中国区域地质,1999,18(1):73－79.
    [19]
    朱日祥,杨振宇,吴汉宁,等.中国主要地块显生宙古地磁视移曲线与地块运动[J].中国科学(D),1998,28(增刊):1－16.
    [20]
    徐树桐,苏文,刘贻灿.大别山北部榴辉岩的发现及其岩相学特征[J].科学通报,1999,44:1452－1456.
    [21]
    王椿镛,张先康,丁志峰,等.大别造山带上部地壳结构的有限差分层析成像[J].地球物理学报,1997,40(4):495－502.
    [22]
    史大年,姜枚,彭聪,等.大别造山带东部地壳结构的层析成像及广角反射的地震学研究[J].地震学报,1999,21(4):403－410.
    [23]
    赵宗举,杨树锋,周进高,等.合肥盆地逆掩冲断带地质——地球物理综合解释及其大地构造属性[J].成都理工学院学报,2000,27(2):151－157.
    [24]
    赵宗举,杨树锋,陈汉林,等.合肥盆地基底构造属性[J].地质科学,2000,35(3):288－296.
    [25]
    徐树桐,陈冠宝,周海渊,等.徐-淮推覆体[J].科学通报,1987,321(4):1091－1095.
    [26]
    李曙光.大陆俯冲化学地球动力学[J].地学前缘,1998,5(4):211－234.
    [27]
    徐佩芬,孙若昧,刘福田,等.扬子板块俯冲、断离的地震层析成像证据[J].科学通报,1999,44(15):1658－1661.
    [28]
    葛宁洁,孙卫东,王兆荣.大别山超高压变质岩三期抬升的年代学证据[J].地球学报——中国地质科学院院报,1997,18(增刊):71－73.
    [29]
    王清晨,林伟.大别山碰撞造山带的地球动力学[J].地学前缘,2002,9(4):257－265.
    [30]
    李忠,李任伟,孙枢,等.合肥盆地南部侏罗系砂岩碎屑组分及其物源构造属性[J].岩石学报,1999,15(3):438－445.
    [31]
    李任伟,李忠,江茂生,等.合肥盆地碎屑石榴石组成及其对源区恢复和地层对比的意义[J].中国科学(D辑 地球科学),2000,30(增刊):91－98.
    [32]
    朱光,徐嘉炜,刘国生,等.下扬子地区沿江前陆盆地形成的构造控制[J].地质论评,1998,44(2):120－129.
    [33]
    闫吉柱,俞凯,赵曙白,等.下扬子区中生代前陆盆地[J].石油实验地质,1999,21(2):95－99.
    [34]
    周进高,赵宗举,邓红婴.合肥盆地构造演化及其含油气性分析[J].地质学报,1999,73(1):15－23.
    [35]
    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.
    [36]
    许长海,周祖翼,马昌前,等.大别造山带140～85Ma 热隆伸展作用——年代学约束[J].中国科学(D辑 地球科学),2001,31(11):925－937.
    [37]
    陈廷愚,牛宝贵,刘志刚,等.大别山腹地燕山期岩浆作用和变质作用物同位素年代学研究及其地质意义[J].地质学报,1991,65(4):329－336.
    [38]
    简平,马昌前,杨坤光.大别造山带东部燕山晚期区域变质－岩浆活动与区域构造抬升的同位素地质年代学证据[J].地球科学——中国地质大学学报,1996,21(5):519－523.
    [39]
    徐启东,张本仁,单光祥,等.大别造山带中生代花岗岩类成分的时空分布与造山带演化的关系[J].地球科学——中国地质大学学报,1997,22(6):595－598.
    [40]
    杨祝良,沈加林,沈渭洲,等.北淮阳中生代火山侵入岩同位素年代学研究[J].地质论评,1999,45(增刊):674－680.
    [41]
    桑隆康,王人镜,张泽明,等.九资河-天堂寨地区燕山晚期花岗岩与大别造山带核部隆升[J].地质学报,2000,74(3):234－246.
    [42]
    杨坤光,马昌前,许长海,等.北淮阳构造带与大别造山带的差异性隆升[J].中国科学(D辑 地球科学),1999,29(2):97－103.
    [43]
    易万霞,赵宗举,李学田,等.早白垩世合肥盆地性质及含油气性分析[J].大地构造与成矿学,2003,27(1):64－71.
    [44]
    李玉发,姜立富,孙乘云,等.安徽省岩石地层——全国地层多重划分对比研究(34)[M].武汉:中国地质大学出版社,1997.
    [45]
    高大旗.安徽磨子潭-晓天地区中生代火山岩的时空分布及火山喷发旋回[J].安徽地质,1992,2(3):20－27.
    [46]
    朱光,徐嘉炜,孙世群.郯庐断裂带平移时代的同位素年龄证据[J].地质论评,1995,41(5):452－456.
    [47]
    Engebretson D C,Cox A,Gordon R G.Relative motions between oceanic and continental plates in the Pacific basin[J].The Geological Society of America,1985,Special Paper 206:1－59.
    [48]
    李显武,周新民.中国东南部晚中生代俯冲带探索[J].高校地质学报,1999,5(2):164－169.
    [49]
    Pearce J A,Deng Wanming.The ophiolites of the Tibet Geotraverse,Lhasa to Golmud(1985) and Lhasa to Kathmandu(1986)[A].Chang C,et al.The Geological Evolution of Tibet[C].London:The Royal Society,1988.215－238.
    [50]
    Pelletier B,Stephan J F.Middle miocene obduction and late Miocene beginning of collision registered in the Hengchun Peninsula:geodynamic implications for the evolution of Taiwan[J].Tectonophysics,1986,125:133-160.
    [51]
    Teng L S.Geotectonic evolution of late Cenozoic arc-continent collision in Taiwan[J].Tectonophysica,1990,183:57－76.
    [52]
    朱光,刘国生,朱漫兰,等.郯庐断裂带晚第三纪以来的浅部挤压活动与深部过程[J].地震地质,2002,24(2):265－277.
    [53]
    周祖翼,许长海,Reiners P W,等.大别山天堂寨地区晚白垩世以来剥露历史的(U-Th)/He和裂变径迹分析证据[J].科学通报,2003,48(6):598－602.
    • Relative Articles
    • Supplements(0)
    • Cited By
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索
    Citation
    XML
    PDF-CN

    Article Metrics

    Article views (675) PDF downloads(479) Cited by()
    Proportional views
    Related

    Website Copyright © Wuxi Research Institute of Petroleum Geology, SINOPEC 苏ICP备15009037号 苏公网安备32021102000780号

    Address：No. 2060, Lihu Avenue, Wuxi, Jiangsu   (214126) Tel：0510-68787204，68787203 Fax：0510-68787113 Email：sysydz.syky@sinopec.com

    Supported by: Beijing Renhe Information Technology Co. Ltd    

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return