收稿日期: 2003-09-30
修回日期: 2004-07-20
网络出版日期: 2005-04-25
基金资助
国家自然科学基金重点项目“山东半岛和朝鲜半岛造山带和克拉通基底对比研究”(编号:40234050);中国科学院知识创新工程重大项目“华北东部中生代构造转折和战略资源预测”(编号:KZCX1-07)资助.
PETROLOGY OF RODINGITES AND THEIR PETROGENETICAL SIGNIFICANCE
Received date: 2003-09-30
Revised date: 2004-07-20
Online published: 2005-04-25
翟明国 , 周磊 , 赵太平 , 倪志耀 . 异剥钙榴岩及其岩石成因意义[J]. 地球科学进展, 2005 , 20(4) : 407 -413 . DOI: 10.11867/j.issn.1001-8166.2005.04.0407
The rodingites are a kind of special metasomatite ,and mostly related to serpentinised ultramafic rocks. They are the result of calcic metasomatism between calcium-rich fluid and related rocks during serpentinization. The serpentinised ultramafic rocks are either end-members of ophiolite or other genetical ultramafic rocks such as Archaean greenstone, Alaskan or Alpine-type rocks, and the rock type may be the dunite,harzburgite and pyroxenite. The formation of rodingites depends on the serpentinization and degree of calcic metasomatism,and has no relationship for genetical types,tectonic setting and age of ultramafic rocks.The viewpoint that rodingites are the end-member of ophiolite or the auxiliary sign for ophiolite discrimination needs to be corrected.
Key words: Rodingites; Ultramafic rock; Serpentinization; Calcic metasomatism.
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