鲁西地区中生代穹盆构造与东亚构造体制转换
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摘要
根据野外观察分析,综合前人研究成果,对鲁西地区中生代褶皱叠加期次、构造特征以及动力学机制进行了分析。结果表明,鲁西中生代构造期次主要分为印支期和燕山期两幕褶皱-逆冲推覆作用,印支期主要为近东西向的宽缓褶皱,燕山期则以北东—北北东向的逆冲推覆和相关褶皱为主,两期褶皱叠加,形成穹盆构造。鲁西地区这种穹盆构造是东亚构造体制转变的地壳变形构造特征的产物。中生代以来,华北和华南地块之间的拼合构成了最初的东亚大陆,主要以近东西向构造为主。中生代中晚期逐渐发育起来的北北东向的环太平洋构造带叠加在东亚大陆的东缘,意味着在这期间古特提斯构造域为主导的汇聚体制转变为古太平洋构造域的俯冲消减体制。
According to field observation and previous research results,this paper makes a detailed study on fold superposition as well as structural styles and geodynamics in Western Shandong Province.The Mesozoic tectonic deformation in the region can be obviously divided into two groups,i.e.the Indosinian EWstriking open to tight folds and related reverse faults and the Yanshanian NNE-or NS-striking box fold and related propagating thrust fault system.The dome-basin structures in this region are the results of the superposition of the Indosinian and Yanshanian folds and represent the crustal deformation related to a transition of the geodynamic systems.The tectonic blocks of Yangtze,North China and Siberian assembled in Mesozoic,and then the East Asia formed,that resulted in the formation of EW-striking structures.Until the middle and late Mesozoic,the NNE-striking circum-Pacific tectonic belt gradually developed and began to affect the eastern margin of the East Asia Continent,Then happened the transition from the collisional systems of the Paleo-Asian Ocean and Paleo-Tethys tectonic domains to the the subduction system of the Paleo-Pacific Tectonic Domain.
According to field observation and previous research results,this paper makes a detailed study on fold superposition as well as structural styles and geodynamics in Western Shandong Province.The Mesozoic tectonic deformation in the region can be obviously divided into two groups,i.e.the Indosinian EWstriking open to tight folds and related reverse faults and the Yanshanian NNE-or NS-striking box fold and related propagating thrust fault system.The dome-basin structures in this region are the results of the superposition of the Indosinian and Yanshanian folds and represent the crustal deformation related to a transition of the geodynamic systems.The tectonic blocks of Yangtze,North China and Siberian assembled in Mesozoic,and then the East Asia formed,that resulted in the formation of EW-striking structures.Until the middle and late Mesozoic,the NNE-striking circum-Pacific tectonic belt gradually developed and began to affect the eastern margin of the East Asia Continent,Then happened the transition from the collisional systems of the Paleo-Asian Ocean and Paleo-Tethys tectonic domains to the the subduction system of the Paleo-Pacific Tectonic Domain.
引文
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