He Zhiliang, Wang Xinwei, Li Shuangjian, Wo Yujing, Zhou Yan. Yanshan Movement and its influence on petroleum preservation in middle-upper Yangtze region[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2011, 33(1): 1-11. doi: 10.11781/sysydz201101001
Citation: He Zhiliang, Wang Xinwei, Li Shuangjian, Wo Yujing, Zhou Yan. Yanshan Movement and its influence on petroleum preservation in middle-upper Yangtze region[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2011, 33(1): 1-11. doi: 10.11781/sysydz201101001

Yanshan Movement and its influence on petroleum preservation in middle-upper Yangtze region

doi: 10.11781/sysydz201101001
  • Received Date: 2010-09-07
  • Rev Recd Date: 2010-12-28
  • Publish Date: 2011-02-28
  • Based on systemic researches on unconformity,tectonic dating and deformation of Jurassic and Cretaceous in different locations of the middle-upper Yangtze region,the Yanshan Movement was divided into 4 stages:the end of Middle Jurassic(Ⅰ),the end of Late Jurassic to the beginning of Early Cretaceous(Ⅱ),the end of Early Cretaceous(Ⅲ)and the Late Cretaceous(Ⅳ),among which the stage Ⅱ was the main deformation stage.The Yanshan Movement was significant for tectonic transformations in the middle-upper Yangtze region.Tectonic movements during the early stages(Ⅰ and Ⅱ)were characterized by multi-direction compression and thrusting,while those of the late stages(Ⅲ and Ⅳ)held the structural features of 'western compressing vs.eastern extending' with differences in basin-mountain relationship,deformation pattern and geodynamic mechanism.Meanwhile,the stage Ⅱ had controlling effects on hydrocarbon preservation in the study area.It caused differences in uplifting-subsiding and marine facies hydrocarbon preservation,and further influenced exploration potential in diffe-rent structural belts.For example,the Sichuan Basin which continued subsiding was favorable for hydrocarbon preservation,and had experienced 3 accumulation stages:early reservoir,conversion from oil to gas,and late adjustment.The fold-thrust belt on the upper Yangtze margin which continued uplifting and eroding was unfavorable for hydrocarbon preservation,and had experienced 2 accumulation stages:early reservoir as well as late reconstruction and destruction.The middle Yangtze region developed to depositional system of tectonic rift within mainland after the stage Ⅱ.Its hydrocarbon preservation conditions lay in the sealing capacity of re-type continental caps and the accumulation was limited by the-effectiveness of secondary hydrocarbon generation.The upper and lower combinations in the Sichuan Basin are the most potential exploration targets.On the margin of Central Guizhou Uplift and in the western Hunan and Hubei region to the east of Qiyueshan Fault,the lower combination below the Cambrian gypsum layers may have some exploration prospects.In the southern depression of the Jianghan Basin,conditions for secondary hydrocarbon generation,late accumulation and preservation may be good under continental covers.

     

  • loading
  • [1]
    Wong W H.Crust movement in eastern China[C]//Proceedings of 3th Pan-Pacific Science Congress.Tokyo:[s.n.].1926:642-685.
    [2]
    黄汲清.中国地质构造基本特征的初步总结[J].地质学报,1960,40(1)1-37.
    [3]
    任纪舜,王作勋,陈炳蔚,等.中国及邻区大地构造图(1/500万)及简要说明书:从全球看中国大地构造[M].北京:地质出版杜,1999;6-9.
    [4]
    吴根耀.燕山运动和中国大陆晚中生代的活化[J].地质科学,2002,37(4):453-461.
    [5]
    董树文,张岳桥,龙长兴,等.中国侏罗纪构造变革与燕山运动新诠释[J].地质学报,2007,81(11):1449-1461.
    [6]
    何治亮,高山林.中国西部燕山运动及其对油气成藏的控制[J].石油与天然气地质,2008,29(4):419-427.
    [7]
    沃玉进,汪新伟.中上扬子地区地质结构类型与海相层系油气保存意义[J].石油与天然气地质,2009,30(2):177-187.
    [8]
    王金琪.安县构造运动[J].石油与天然气地质,1990.11(3):223-234.
    [9]
    徐亚军,杨坤光,马昌前.秦岭地区城口一房县断裂带变形特征及ESR定年[J].现代地质,2005,19(1):127-132.
    [10]
    王岳军,李三忠,陈世悦,等.雪峰陆内推滑构造系统与油气藏保存研究[R].北京:中国石化科技开发部,中科院广州地球化学研究所,2009.
    [11]
    刘少峰,颜丹平,于炳松,等.中上扬子中新生代构造演化与上组合研究[R].北京:中国石化科技开发部,中国地质大学(北京),2009.
    [12]
    汪新伟,沃玉进,周雁,等.上扬子地区褶皱-冲断带的运动学特征[J].地学前缘,2010,17(3):200-212.
    [13]
    丁道桂,朱樱,陈风良,等.中、下扬子区占生代盆地基底拆离式改造与油气领域[J].石油与天然气地质,1991,12(4):376~384.
    [14]
    赵宗举,俞广,朱琰,等.中国南方大地构造演化及其对油气的控制[J].成都理工大学学报(自然科学版),2003,30(2):155-168.
    [15]
    戴少武.江汉盆地印支期以来区域构造特征探讨[J].地质力学学报,1996,2(4):80-84.
    [16]
    赵泽恒,张桂权,薛秀丽.黔中隆起下组合古油藏和残余油气藏[J].天然气工业,2008,28(8):39-42.
    [17]
    向才富,汤良杰,李儒峰,等.叠合盆地幕式流体活动:麻江古油藏露头与流体包裹体证据[J].中国科学(D),2008,38(增Ⅰ):70-77.
    [18]
    赵宗举,冯加良,陈学时,等.湖南慈利灯影组古油藏的发现及意义[J].石油与天然气地质,2001.22(2):114-118.
    [19]
    凡元芳,丰勇.南山坪古油藏的形成及其破坏因素分析[J].矿产与地质,2005,19(3):296-298.
    [20]
    刘光祥,王守德,潘文蕾,等.四川广元天井山古油藏剖析[J].海相油气地质,2003.8(1-2);103-107.
    [21]
    蔡立国,饶丹,潘文蕾,等.川东北地区普光气田成藏模式研究[J].石油实验地质,2005,27(5):462-467.
    [22]
    刘树根,马永生,孙玮,等.四川盆地威远气田和资阳含气区震旦系油气成藏差异性研究[J].地质学报,2008.82(3):328-337.
    [23]
    马永生,傅强,郭彤楼,等.川东北地区普光气田长兴飞仙关气藏成藏模式与成藏过程[J].石油实验地质,2005,27(5):455-461.
    [24]
    姚雪根.四川盆地天然气成藏条件及其勘探方向[J].海相油气地质,2002,7(1):13-28.
    [25]
    饶丹,徐国盛,邱蕴玉.苏北盆地朱家墩气田气源追溯[J].成都理工大学学报,2006,33(4):394-401.
  • 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

    Article Metrics

    Article views (3270) PDF downloads(1059) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return