Geological Characteristics of Igneous Rocks Distributed in <?xml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:State w:st="on">Gansu</st1:State> Section of Subnorth Belt of <st1:place w:st="on"><st1:PlaceName w:st="on">Beishan</st1:PlaceName> <st1:PlaceType w:st="on">Mountain</st1:PlaceType></st1:place> Located in Border of Gansu-Xinjinag-Mongolia <?xml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" /><o:p></o:p>

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Geological Characteristics of Igneous Rocks Distributed in Gansu Section of Subnorth Belt of Beishan Mountain Located in Border of Gansu-Xinjinag-Mongolia

详细信息

责任者：Sun Xinchun (Geological Survey of Gansu Province ; Lanzhou 730000 ; China) ; Cheng Yuchen
刊名：Gansu Geology
出版年：2009
卷期：18(3)
关键词：火成岩 ; igneous rocks ; 甘肃 ; Gansu Province
页码：p.8-13, 31
图表：5 illus., 1 table, 2 refs.
分类号：0801
issnNo：ISSN1004-4116
isbnNo：CN 62-1191/P

摘要

///Survey area lies in Subei County of Gansu Privince, tectonicaly belongs to Sidingbishan-Queershan magatic arc belt in Paleozoic which situated on the east-south margin of Kazabstan paleoplate. It tends to nearly east-west direction. Its material compositions there are the Paleozoic strata, the intrusive rocks in Triassic and Carboniferous, and the main fault in the north of Sidingbishanshuang goushan. The intrusive rocks include Triassic Xiaocaohu superunit and manshan superunit, Paleozoic Ganheliang superunit, Carboniferous-Paleozoic Sidinghishan sequences, Shuarggoushan sequences and Dayushan sequences, Carboniferous, Sidinghishan basic-ultrabasic rocks.

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