Article ID Journal Published Year Pages File Type
9528431 Marine and Petroleum Geology 2005 14 Pages PDF
Abstract
Surface indications suggest that the structure has been active until the present day. Elevations of a bedding plane on the Shedgum plateau reveal a 0.25° dip angle, which cannot be distinguished on the surface by the human eye. The movements that occurred during the 4 million years since the Pliocene period reveal an average tilting of 0.06° per one million years.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Economic Geology
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