松辽盆地上古生界区域地层对比研究
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摘要
松辽盆地上古生界地层一直被认为是海西期褶皱带或碰撞造山带,长期以来被作为盆地的变质结晶基底而成为油气勘查的禁区。随着近些年来研究进展,提出的盆地深部上古生界具有油气资源前景这一认识的深化,提出了"佳蒙地块"的新认识,改变了对该区传统大地构造观(即褶皱造山带)的认识(王成文等,2008a,b,2009a,b),发现东北地区上古生界以海相沉积为主,并没有遭受强烈区域变质作用。本文结合松辽盆地已有钻井资料、区域构造事件、深大地震剖面、非震地球物理资料的解释成果及盆地周边基岩区上古生界地层厚度,综合标定松辽盆地北部上古生界顶底界面,查明了松辽盆地上古生界总体展布特征,为下一步的油气勘探计划提供理论依据。
引文
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[2]王成文,马志红,孙跃武,等.晚古生代海相地层——东北地区油气勘查的一个新层系[J].世界地质,2008b,27(2):113-118.WHANG Cheng-wen,MA Zhi-hong,SUN Yue-wu,et al.Late Paleozoic marine strata:a new layer for oil-gas exploration in Northeast China[J].global geology,2008b,27(2):113-118.
[3]王成文,孙跃武,李宁,等.东北地区晚古生代地层分布规律[J].地层学杂志,2009,33(1):56-61.WHANG Cheng-wen,SUN Yao-wu,LI Ning,et al.On the distribution of Late Paleozoic strata in Northeast China[J].Journal of Stratigraphy,2009,33(1):56-61.
[4]王成文,孙跃武,李宁,等.中国东北及邻区晚古生代地层分布规律的大地构造意义[J].中国科学:D辑,2009,39(10):1429-1437.WHANG Cheng-wen,SUN Yao-wu,LI Ning,et al.Tectonic implications of Late Paleozoic stratigraphic distribution in Northeast China and adjacent region[J].Science in China:Ser D,2009,39(10):1429-1437.
[5]张兴洲,周建波,迟效国,等.东北地区晚古生代构造-沉积特征与油气资源[J].吉林大学学报:地球科学版,2008,38(5):719-725.ZHANG Xing-zhou,ZHOU Jian-bo,CHI Xiao-guo,et al.Late Paleozoic Tectonic Sedimentation and Petroleum Resources in Northeastern China[J].Journal of Jilin University:Earth Science Edition,2008,38(5):719-725.
[6]张兴洲,乔德武,迟效国,等.东北地区晚古生代构造演化及其石油地质意义[J].地质通报,2011,30(2-3):205-213.ZHANG Xing-zhou,QIAO De-wu,CHI Xiao-guo,et al.Late-Paleozoic tectonic evolution and oil-gas potentiality in northeastern China[J].Geological Bulletin of China,2011,30(2-3):205-213.
[7]乔德武,任收麦,邱海峻,等.中国油气资源勘探现状与战略选区[J].地质通报,2011,30(2-3):187-196.QIAO De-wu,REN Shou-mai,QIU Hai-jun,et al.The present situation of oil&gas resources exploration and strategic selection of potential area in China[J].Geological Bulletin of China,2011,28(2/3):187-196.
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