Geochemistry of Layered Ultramafic Rocks in J.C. Pura Schist Belt, Dharwar Craton, Karnataka, India
نویسندگان
چکیده
The Jayachamarajapura schist belt in western Dharwar craton, southern India, is predominantly an ultramafics dominant terrain. These rocks have been extensively metamorphosed and altered to serpentinite. komatiite nature of conspicuous. In most the areas these are massive nature. However, some ultramafic units show layered But, their outcrops encompassed within komatiitic bodies. Mg-rich also Mg-rich, field setting geochemistry suggest intermittent occurrence as sills, during differentiation peridotitic magma. rocks, which intensely serpentinisation homogenous They almost wholly made serpentine with occasional relics pyroxene. Secondary carbonate mineral often noticed. Their higher MgO content indicates magmatism Archaean orogeny.
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ژورنال
عنوان ژورنال: Open Journal of geology
سال: 2023
ISSN: ['2161-7589', '2161-7570']
DOI: https://doi.org/10.4236/ojg.2023.132009