2010Journal of Southwest University of Science and TechnologyRequires access

The Discovery of the Unconformity on Upper Carboniferous in the Southern Qiaerlong,Akto County,Xinjiang

Lanjie Hou

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Abstract

During 15 million regional geological survey,the authors found that there was a unconformity at the top of Keying group in Qiaerlongnan.The unconformity was manifested as the paleo-weathering crust,basal conglomerate,sequence missing and strata chemical abnormal.The study shows,for sea level relative decline in Sinian-Devonian,it is caused by sedimentary interruption in sedimentary facies evolution-coastal-neritic phase to sedimentary basin.That reflects the unconformity's sxistent by data of measured sections,geological mapping,chemical strata and paleo-geographic framework.The discovery has important significance of elucidating sequence stratigraphic framework and evolution of paleogeography in carboniferous,west Kunlun,and denies the statement about regional fault with predecessors.

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What this paper is about

During 15 million regional geological survey,the authors found that there was a unconformity at the top of Keying group in Qiaerlongnan.The unconformity was manifested as the paleo-weathering crust,basal conglomerate,sequence missing and strata chemical abnormal.The study shows,for sea level relative decline in Sinian-Devonian,it is caused by sedimentary interruption in sedimentary facies evolution-coastal-neritic phase to sedimentary basin.That reflects the unconformity's sxistent by data of measured sections,geological mapping,chemical strata and paleo-geographic framework.The discovery has important significance of elucidating sequence stratigraphic framework and evolution of paleogeography in carboniferous,west Kunlun,and denies the statement about regional fault with predecessors.

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Available abstract

During 15 million regional geological survey,the authors found that there was a unconformity at the top of Keying group in Qiaerlongnan.The unconformity was manifested as the paleo-weathering crust,basal conglomerate,sequence missing and strata chemical abnormal.The study shows,for sea level relative decline in Sinian-Devonian,it is caused by sedimentary interruption in sedimentary facies evolution-coastal-neritic phase to sedimentary basin.That reflects the unconformity's sxistent by data of measured sections,geological mapping,chemical strata and paleo-geographic framework.The discovery has important significance of elucidating sequence stratigraphic framework and evolution of paleogeography in carboniferous,west Kunlun,and denies the statement about regional fault with predecessors.

Key concepts: Unconformity, Geology, Conglomerate, Carboniferous, Sedimentary rock, Paleontology, Facies, Fault (geology)

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The Discovery of the Unconformity on Upper Carboniferous in the Southern Qiaerlong,Akto County,Xinjiang — Research Paper | ScholarLens