渤海湾盆地区晚中生代以来大陆岩石圈伸展模式
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摘要
<正>1.引言核杂岩、宽裂谷、窄裂谷这3种大陆伸展模式已被人所熟知。而且,前人采用地壳厚度、热流密度和岩石圈伸展速率这3个参数对大陆岩石圈的伸展模式进行了描述和数值模拟~([1-3])。本文通过整理渤海湾盆地区的相关数据,对比其岩石圈晚中生代以来的伸展模式。2.岩石圈伸展模式
引文
1.Buck W R.Models of continental lithospheric extension.Journal of Geophysical Research,1991,96(B12):20,161-20,178.
    2.Schubert,G.Treatise on geophysics.Elsevier Science,2007,325-379.
    3.Nagel T J,et al.Control of rheological stratification on rifting geometry:a symmetric model resolving the upper plate paradox.Journal of Earth Science,2007,96:1047-1057.
    4.付明希,等.华北东部中生代热体制转换及其构造意义.中国科学(D辑),2004,34(6):514-520.
    5.朱日祥,等.华北克拉通破坏.中国科学(D辑),2012,42(8):1135-1159.
    6.Qiu N S,et al.Geothermal evidence of Meso-Cenozoic lithosphere thinning in the Jiyang sub-basin,Bohai Bay Basin,eastern North China Craton.Gondwana research,2014,26(3-4):1079-1092.
    7.黄清华,等.中国地球科学联合学术年会论文集.中国和平音像电子出版社,2014,422-422.
    8.龚育龄,等.济阳坳陷大地热流分布特征.中国科学(D辑),2003,33(4):384-391.
    9.Sugisaki R.Chemical characteristics of volcanic rocks:Relation to plate movements.Lithos,1976,9:17-30.
    10.万天丰.山东省构造演化与应力场研究.山东地质,1992,8(2):70-101.
    11.王盘喜,等.冀中坳陷火成岩岩石学及地球化学特征.地质科技情报,2012,31(4):1-10.
    12古团,等.辽河盆地新生代火山岩地球化学特征及其与油气成藏的关系.矿物学报,2006,26(3):325-334.
    13.张超,等.渤海湾黄哗盆地晚中生代-新生代火山岩地球化学岩石成因及构造体制转换.岩石学报,2009,25(5):1159-1177.
    14.Li H Y,et al.Geochemistry of Cenozoic basalts from the Bohai Bay Basin:implications for a heterogeneous mantle source and lithospheric evolution beneath the eastern North China Craton.Lithos,2014,196-197:54-66.
    15.赵国连.济阳凹陷火山岩的岩石学与地球化学.矿物学报,2006,26(3):335-345.
    16.Jiang W L,et al.Detailed crustal structure of the North China and its implication for seismicity.Journal of Asian earth sciences,2014,81:53-64.
    17.魏文博,等.2006.华北地区大地电磁测深及岩石圈厚度讨论.中国地质,33(4):762-772
    18.Chen L,et al.Distinct lateral variation of lithospheric thickness in the Northeastern North China Craton.Earth and Planetary Science Letters,2008,267:56-68.

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