Geology of the petroleum and coal deposits in the North China basin, eastern China

Open-File Report 86-154
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Abstract

The North China basin evolved initially from a rifted intracratonic graben system on the east-central Sino-Korean platform during the Jurassic and Cretaceous Yanshanian orogeny. The basin reached its maximum stage of development in the Neogene owing to rift reactivation by the Himalayan orogeny. As indicated by geophysical data, extensional rifting within the basin is still active today.

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Publication type Report
Publication Subtype USGS Numbered Series
Title Geology of the petroleum and coal deposits in the North China basin, eastern China
Series title Open-File Report
Series number 86-154
DOI 10.3133/ofr86154
Year Published 1986
Language English
Publisher U. S. Geological Survey
Description 57 p.
Country China
Other Geospatial North China basin
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