Rodingite from Oceanic Lithology of Shaliuhe Terrane in North Qaidam UHPM Belt and Its Geological Implication
详细信息
- 责任者：Zhang Guibin (Key Laboratory of Orogenic Belts and Crustal Evolution ; Ministry of Education ; School of Earth and Space Sciences ; Peking University ; Beijing 100871 ; China) ; Zhang Lifei
- 刊名：Earth Science Frontiers
- 出版年：2011
- 卷期：18(2)
- 关键词：超高压变质带 ; ultrahigh pressure metamorphic zones ; 变质岩 ; metamorphic rocks ; 柴达木盆地 ; Qaidam Basin
- 页码：p.151-157
- 图表：4 illus., 1 table, 40 refs.
- 分类号：0802
- 出版序号：20120197
- issnNo：ISSN1005-2321
- isbnNo：CN11-3370/P
摘要
Rodingite, coexisting with serpentinized harzburgite,was found in the Shaliuhe ophiolite sequence, North Qaidam UHPM belt. It is mainly composed of grossular, dioposide, chlorite, carbonate and minor prehnite, zoisite. Rodingite is a typical product of ocean-floor metamorphism. The Shaliuhe rodingite is the second evidence for the oceanic subduction in North Qaidam UHPM belt.
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