Advanced Search
Volume 28 Issue 1
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2006  >  28(1): 1-7
Huang Zeguang, Gao Changlin. VOLCANIC ROCKS AND FOREDEEP BASIN IN MESOZOIC, THE SOUTHERN NORTH CHINA[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2006, 28(1): 1-7. doi: 10.11781/sysydz200601001
Citation: Huang Zeguang, Gao Changlin. VOLCANIC ROCKS AND FOREDEEP BASIN IN MESOZOIC, THE SOUTHERN NORTH CHINA[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2006, 28(1): 1-7. doi: 10.11781/sysydz200601001
shu

VOLCANIC ROCKS AND FOREDEEP BASIN IN MESOZOIC, THE SOUTHERN NORTH CHINA

doi: 10.11781/sysydz200601001
  • 1.

    School of Oceanic Geology and Geosciences, Tongji University, Shanghai 200092, China

  • 2. Wuxi Research Institute of Petroleum Geology, Research Institute of Petroleum Exploration and Production, SINOPEC, Wuxi, Jiangsu 214151, China

  • Received Date: 2005-11-01
  • Publish Date: 2006-01-28
    Abstract
  • Volcanic rocks have been studied with geochemical theory and method in Mesozoic,the southern North China.The rock types include andesite-basalt,andesite,dacite,liparite which are calic-alkalic and alkalic,high-K,high-∑REE and rich in LREE.The forming tectonic environment of volcanic rocks is not related to plate subduction-collision or rifting,but mantle plume after plate subduction-collision.The forming tectonic environment of Hefei and Zhoukou is related to thermo-extension.The tectonic framework is controlled by mantle plume action(140～85 Ma).The space style of tectonic unites is composed of thermal dome-detachment fault-sliding system.The basin is formed in sliding system and the basin type is foredeep.

     

    • FullText(HTML)
  • loading
    • References(36)
  • [1]
    胡居文.华北地区中生代盆地与油气[J].石油与天然气地质,1989,10(4):378～391.
    [2]
    张功成,王定一,吕锡敏.南华北中、新生代盆地构造特征[A].见:张功成,徐宏编.中国含油气盆地构造[C].北京:石油工业出版社,1999.201～212.
    [3]
    何明喜.东秦岭(河南部分)新生代拉伸造山作用与盆岭伸展构造[M].西安:西北大学出版社,1995.53～116.
    [4]
    孙肇才.板内形变与晚期成藏[M].北京:地质出版社,2003.43～50.
    [5]
    袁政文,何明喜,宋建华等.周口残留盆地油气勘探前景分析[J].石油实验地质,2004,25(6):679～684.
    [6]
    吕俊祥,黄泽光.南华北地区中新生代盆地成盆环境分析[J].石油实验地质,2005,27(2):118～123.
    [7]
    杜建国,张鹏.大别山造山带北部的中生代火山岩[J].现代地质,1999,13(1):57～65.
    [8]
    童亨茂.中国沉积盆地复杂性的成因剖析及其油气赋存特征[J].石油实验地质,2004,26(5):415～421.
    [9]
    赵宗举.合肥盆地与大别-张八岭造山带的耦合关系[J].石油实验地质,2003,25(6):670～678.
    [10]
    吴根耀.中国东部燕山期高原的发育及对矿产和油气资源评价的启示[J].石油实验地质,2002,24(1):3～12.
    [11]
    许长海,周祖翼,马昌前等.大别造山带140～85 Ma热窿伸展作用—年代学约束[J].中国科学(D辑),2001,31(11):925～937.
    [12]
    邱家骧,林景仟.岩石化学[M].北京:地质出版社,1991.100～101.
    [13]
    Rittmann A.火成岩的稳定矿物组合计算方法[M].金秉慧译.北京:地质出版社,1979.1～55.
    [14]
    Gill J B.Orogenic andesites and plate tectonics[M].Berlin:Springer-Verlag,1981.1～90.
    [15]
    Thorpe R S,Potts P J,Francis P W.Rare earth data and petrogenesis of andesite from the north Chilenan Andes[J].Contrib Mineral Petrol,1976,54:65～78.
    [16]
    Whitford D J.Spatial variations in the geochemistry of Quaternary lavas across the Sunda arc in Java and Bali[J].Contrib Mineral Petrol,1979,70:341～356.
    [17]
    从柏林.岩浆活动与火山岩组合[M].北京:地质出版社,1979.1～185.
    [18]
    勒夫勒 H K.含SiO2低于43%的岩石里特曼"系列指数"的修正[J].地质地球化学,1980,(10):48～50.
    [19]
    索书田,钟增球,游振东.大别地块超高压变质期后伸展变形及超高压变质岩石折返过程[J].中国科学(D辑),2000,30(1):9～17.
    [20]
    王国灿,杨巍然.大别造山带中新生代隆升作用的时空格局—构造年代学证据[J].地球科学,1996,21(5):524～528.
    [21]
    杨坤光,马昌前.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),1999,29(2):97～103.
    [22]
    宋明水.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.
    [23]
    张云银.郯庐断裂带含油气性研究[J].石油实验地质,2003,25(1):28～32.
    [24]
    余和中,吕福亮.华北板块南缘原型沉积盆地类型与构造演化[J].石油实验地质,2005,27(2):111～117.
    [25]
    曹高社.合肥盆地中—新生界烃源岩地球化学与构造背景分析[J].石油实验地质,2004,26(3):287～291.
    [26]
    吉让寿,刘光祥,潘文蕾等.试论前陆—伸展盆地[J].石油实验地质,2003,25(增刊):539～542.
    [27]
    高长林,刘光祥,张玉箴等.东秦岭—大巴山逆冲推覆构造与油气远景[J].石油实验地质,2003,25(增刊):523～531.
    [28]
    谈彩萍,刘翠荣.中国东部老油区油气成藏特征[J].石油实验地质,2005,27(2):144～150.
    [29]
    全书进.周口坳陷上古生界油气资源潜力分析[J].石油实验地质,2004,26(6):542～546.
    [30]
    闫吉柱.下扬子区中生代前陆盆地[J].石油实验地质,1999,21(2):95～99.
    [31]
    汪新文,陈发景,李光等.塔北库车坳陷的变形特征及其与油气关系[J].石油与天然气地质,1994,15(1):40～50.
    [32]
    高长林,叶德燎,张玉箴等.塔里木中新生代盆地扩张和盆地俯冲与地幔柱[J].石油实验地质,2003,25(6):661～669.
    [33]
    刘志宏,卢华复,贾承造等.库车再生前陆盆地的构造与油气[J].石油与天然气地质,2001,22(4):297～303.
    [34]
    高长林.前陆盆地的类型及油气远景[J].石油实验地质,2000,22(2):99～104.
    [35]
    车自成,刘良,罗金海.中国及其邻区域大地构造学[M].北京:科学技术出版社,2002.1～515.
    [36]
    高长林,黄泽光,张玉箴.周口白垩系砂泥岩的化学特征及其构造学意义[J].石油天然气地质,2005,26(2):237～241
    • 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 (533) PDF downloads(414) 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