摘要
跃进山群出露位于佳木斯地块和那丹哈达地体之间，是完达山造山带的组成部分。它由大陆斜坡相沉积物、大洋中脊型玄武岩和洋岛型玄武岩组成，其中有镁铁－超镁铁质岩块体。它不是一个地层单位。
The Yuejinshan Group lies between Jiamusi and Nadanhada terranes and is a part of the Wandashan orogenic belt. It is composed of continental slope mass, MORB and OIB, with some mafic ultramafic blocks. It is not a stratigraphic unit, but an ophiolite melange relating to subduction in active continent margin.
出处
《岩石学报》
SCIE
EI
CAS
CSCD
北大核心
1997年第2期168-172,共5页
Acta Petrologica Sinica
基金
国家自然科学基金
关键词
绿片岩
跃进山群
地球化学特征
地质意义
Green schist
Yuejinshan Group
Geochemical Characteristics
Heilongjiang PreovinceXia Xuehui (Geological Institute for Chemical Minerals, Ministry of Chemical Industry, Zhuozhou, 072754) Abstract Tourmaline rocks widely occur within the p
