DETRITAL MODES OF THE CRETACEOUS INGIIN NARS SANDSTONES IN THE SAINSHAND BASIN
Keywords:
sandstone, continental block, Cretaceous, diagramAbstract
The Ingiin-Nars properly is located in the southern part of the Sainshand sedimentary Basin. The basins is filled with syn & post riflogenic alluvial, fluvial, and lacustrine and limnic sedimentary rocks of Early to Late Cretaceous age. which are covered by Paleocene to Quaternary alluvium loose sediments. Paleozoic to Jurassic, meta-sedimenls and granites form the basement of the basin. The older sequences were affected by the Caledonian progeny. Basins were down faulted during Cretaceous time. The study sandstone of the Ingiin Nars area is classified as arkosic type. Considering the sandstone modal composition the studied sandstones are derived from continental block orogin.
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Graham S.A., Hendrix M.S., Johnson C.L., Badamgarav D., Badarch G., Amory J., Porter M., Barsbold R., Webb L.E., and Hacker, B.R . 2001, Sedimentary record and tectonic implications of Mesozoic rifling in southeast Mongolia. Geological Society of America Bulletin 113, 1560-1579.
Jargal l., Lee Y. I., Detrital modes of the Fast Gobi Basin (Ondor-Bogd area) sandstones (Late Jurassic- Early Cretaceous) in southeastern Mongolia and their geological implications. Geosciences Journal Vol. 10.1. p. 1-16, March 2006
Miranov U.B. Uran Mongolii, Mockva 2004
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