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松辽盆地北部徐家围子断陷构造格局及其成因 被引量:39
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作者 刘学锋 钟广法 +1 位作者 王正允 陈强 《西安石油大学学报(自然科学版)》 CAS 2006年第4期6-10,共5页
徐家围子断陷形成于晚侏罗—早白垩世早期,是松辽盆地北部深层最重要的生气断陷.运用构造解析的方法,结合地质背景和应力环境分析,对徐家围子断陷的构造格局及其成因进行探讨.断陷期形成的地层中发育有近南北向(北北西、北北东向)伸展... 徐家围子断陷形成于晚侏罗—早白垩世早期,是松辽盆地北部深层最重要的生气断陷.运用构造解析的方法,结合地质背景和应力环境分析,对徐家围子断陷的构造格局及其成因进行探讨.断陷期形成的地层中发育有近南北向(北北西、北北东向)伸展断裂、北东向—北东东向正断层、北北西向逆冲断层、北北西向褶皱、北东向褶皱、北东东向褶皱等多组构造形迹.除北东向褶皱为晚期北西—南东向挤压应力作用的产物,其它构造形迹均形成于断陷期.断陷期地层内发育的3个不整合被解释为断陷期构造幕式渐进变形的产物.徐家围子断陷的两凹一凸的构造格局受近南北向压扭应力场控制,其中平行于最大主压应力方向发育的左旋斜列低角度边界正断层控制了2个箕状断凹的形成,分隔这两个断凹的断凸的形成则与边界断裂的倾滑作用派生的局部挤压应力有关. 展开更多
关键词 松辽盆地 徐家围子断陷 构造构局 倾滑作用 应力环境
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A New (2+1)-Dimensional KdV Equation and Its Localized Structures 被引量:1
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作者 彭彦泽 《Communications in Theoretical Physics》 SCIE CAS CSCD 2010年第11期863-865,共3页
A new (2+1)-dimensional KdV equation is constructed by using Lax pair generating technique. Exact solutions of the new equation are studied by means of the singular manifold method. Bgcklund transformation in terms... A new (2+1)-dimensional KdV equation is constructed by using Lax pair generating technique. Exact solutions of the new equation are studied by means of the singular manifold method. Bgcklund transformation in terms of the singular manifold is obtained. And localized structures are also investigated. 展开更多
关键词 (2+1)-dimensional KdV equation Lax pair generating technique singular manifold method
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Structure and coalbed methane occurrence in tectonically deformed coals 被引量:50
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作者 HOU QuanLin LI HuiJun +4 位作者 FAN JunJia JU YiWen WANG TianKai LI XiaoShi WU YuDong 《Science China Earth Sciences》 SCIE EI CAS 2012年第11期1755-1763,共9页
Research on structure of tectonically deformed coals(TDC) is a key issue in coal and gas outburst prevention and coalbed methane(CBM) exploitation.This paper presents a summary on the research progress in TDC's st... Research on structure of tectonically deformed coals(TDC) is a key issue in coal and gas outburst prevention and coalbed methane(CBM) exploitation.This paper presents a summary on the research progress in TDC's structural-genetic classification,tectonic strain influence on coal microstructure,coal porosity system,coal chemical structure and constituents,and their relationship with the excess coalbed methane.Previous studies suggested that tectonic deformation had significant influence on coal microstructure,coal super microstructure,and even chemical macromolecular structure.The main mechanisms of coal deformation are the tectonic stress degradation and polycondensation metamorphism(dynamical metamorphism).Besides,under different deformation mechanisms,the ultra-and micro-structure and chemical constituents of TDC presented distinct characteristics.Based on these achievements,we propose one possible evolutionary trend of TDC with different deformation mechanisms,and suggest that the coal and gas outburst in the TDC,especially in the mylonitic coals,may be not only controlled by geological structure,but also influenced by the tectonic stress degradation of ductile deformation.Therefore,further study on TDC should be focused on the controlling mechanism of deformation on structure and composition of coal,generation conditions and occurrence state of excess coalbed methane from deformation mechanism of coal. 展开更多
关键词 tectonically deformed coal deformation mechanism coalbed methane occurrence research progress
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