• 责任者：Wang Hongyan (Chinese Academy of Geological Sciences ; Beijing 100037 ; China) ; Zhang Chuanlin
• 刊名：Geological Bulletin of China
• 出版年：2011
• 卷期：30(8)
• 关键词：火山岩 ; volcanic rocks ; 青藏高原 ; Qinghai-Tibetan Plateau
• 页码：p.1171-1181
• 图表：illus., 3 tables, 37 refs.
• 分类号：0801
• issnNo：ISSN1671-2552
• isbnNo：CN11-4648/P

PAN style="FONT-FAMILY: ’Times New Roman’,’serif’" lang=EN-US>A whole-rock ⁴⁰Ar-³⁹Ar age of (0.81±0.21) Ma was obtained for the North Pulu potassic volcanic rocks in the northwestern margin of Tibetan Plateau. The rocks belong to shoshonite series and are mainly composed of shoshonite and trachyandesite. The North Pulu potassic volcanic rocks might have been the product that responded to the delamination of the mantle lithosphere beneath the northwestern margin of the Tibetan Plateau during the Late Cenozoic continent-continent collision orogeny.