Early Paleozoic intracontinental felsic magmatism in the South China Block: Petrogenesis and geodynamics

Lithos3.50
Volume: 234-235, Pages: 79 - 92
Published: Oct 1, 2015
Abstract
Intraplate magmatism is generally anorogenic in nature, characterized by geochemical and isotopic signatures that are indicative of mantle sources. However, the early Paleozoic intracontinental magmatic rocks in the South China Block, which cover an area of ~ 22,000 km2, are mainly granitoids with fertile isotopic signatures. Based on mineral assemblages, these early Paleozoic granitoids are divided into three groups: Group A (amphibole-bearing...
Paper Details
Title
Early Paleozoic intracontinental felsic magmatism in the South China Block: Petrogenesis and geodynamics
Published Date
Oct 1, 2015
Journal
Volume
234-235
Pages
79 - 92
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