地球学报2001，Vol.22Issue(1)：11-16，22,7.
中国超高压变质岩十五年研究进展
Development of Studying Ultrahigh-Pressure Metamorphic
Rocks from China during the Past 15 Years
摘要
Abstract
Studies on the ultra-high pressure metamorphic (UHPM) rocks from China started in 1980s. Progresses so far made in the field could be summarized as follows.① The Dabieshan-Su-Lu UHPM belt has been well-known since many new outcrops of UHPM rocks were found；② Mineralogical evidences indicate that the continental crust rocks with low density could subduct down to depth of >200 km and undergo UHPM；③ UHPM rocks from the Dabieshan-Su-Lu area were dated as early Mesozoic when the Yangtze Craton subducted northward beneath the Sino-Korean Craton； ④ Fluids were not active and oxygen isotope composition of meteoric water could be preserved during UHPM process, as is evidenced by O, C, and H isotope data； ⑤Multistage models were suggested to explain the exhumation of the UHPM terrain. Some hotly debated issues were summarized.关键词
超高压变质岩/中国/大别山-苏鲁分类
天文与地球科学引用本文复制引用
王清晨..中国超高压变质岩十五年研究进展[J].地球学报,2001,22(1):11-16，22,7.
