摘要
武当山地块基性岩墙群的地球化学特征表明，它们为具大陆拉斑玄武岩特征的大陆板内岩浆侵入的产物，是古陆块裂解并保存在造山带内基底岩块中的重要证据，这表明南秦岭和扬子板块曾存在晋宁期固结的统一古陆块，该古陆块在新元古代早期发生了一次重要的裂解作用。
There are a lot of Neo-proterozoic basic dykes in Wudangshan block. The geochemicalfeatures of these basic dykes show that they were the products of intmsion of the continentalwithin-plate magma characterized by continental tholeiitic basalts into the continental plate,which is a very important evidence for the rifting of ancient continental block. Therefore, therewas an ancient continental block in South Qinling and Yangtze area in Jinning period, where animportant rifting occurred in early Neo-proterozoic.
出处
《地球化学》
CAS
CSCD
北大核心
1999年第2期126-135,共10页
Geochimica
基金
国家自然科学基金
关键词
基性岩墙
地球化学
古陆块
武当山块
大地构造
basic dyke, geochemistry, ancient continental block, Wudangshan block
