<P style="MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>The Permian Lithofacies Paleogeographic Characteristics and Basin-Mountain Conversion in the pace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />place w:st="on">Kunlunplace> Orogenic Beltpace prefix = o ns = "urn:schemas-microsoft-com:office:office" />p>p>

详细信息   

• 责任者：Chen Shoujian (Xi’an Institute of Geology and Mineral Resources ; Xi’an 710054 ; China) ; Li Rongshe
• 刊名：Geology in China
• 出版年：2010
• 卷期：37(2)
• 关键词：二叠纪 ; Permian ; 岩相古地理 ; lithofacies paleogeography ; 昆仑山 ; Kunlun Mountains
• 页码：p.374-393
• 图表：11 illus., 6 tables, 46 refs.
• 分类号：1200
• issnNo：ISSN1000-3657
• isbnNo：CN11-1167/P

摘要

<P style="MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto" class=MsoNormal>pt; mso-font-kerning: 0pt" lang=EN-US>The pace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />place w:st="on">Kunlunplace> orogenic belt was basically formed in Paleozoic, resulting from ocean-continent conversion and collision orogenic activity. Based on field work, analytical tests and integrated studies in association with the 1∶250 000 regional geological data and other data available, the authors chose the Permian strata of Late Palaeozoic as the study object and discussed the Permian lithofacies characteristics and tectono-paleogeography with the purpose of improving the research level of the Kunlun orogenic belt.pace prefix = o ns = "urn:schemas-microsoft-com:office:office" />p>p>