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- W2367093592 abstract "The time of ancient land in Ordos Basin is one of important question in science theory and practice.Based on the basic geologic proof,the achievements that were acquired by former geologists,through analyzing geotectonic evolvement and geodynamics characteristics and linking with analysis of sedimentation,with the latest seismic and other data,thought that Western ancient land rise and Yinchuan ancient rise were not found and the both the foreland basin and subside center which ever though were south-north in strike not found,either in late Triassic.The western borderline of the basin may in Main Yanshanian period and made Liupanshan Basin separated from Ordos Basin.In early Cretaceous,Liupanshan mountains were leveled to the ground and Ordos Basin connect with western Cretaceous basin including Liupanshan basin late.The western borderline of the Ordos Basin which can be seen now were formed in Middle-late Himalayan period.Zuozishan mountains Helanshan mountains-Liupenshan mountains(South North ancient land rise) were formed in Middle-late Himalayan period,too.These geological phenomenon were the result of the stress effect of far distance,which were caused by active of both Ocean plate India and Pacific Ocean plate." @default.
- W2367093592 created "2016-06-24" @default.
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- W2367093592 date "2006-01-01" @default.
- W2367093592 modified "2023-09-25" @default.
- W2367093592 title "FORMING AND EVOLUTION OF ANCIENT LAND RISE IN THE WESTERN ORDOS BASIN" @default.
- W2367093592 hasPublicationYear "2006" @default.
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