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Petrology of the Gabbro-Diorite-Syenite-Granite Complex of Chanduluru, Prakasam Alkaline Province, Andhra Pradesh, India


Affiliations
1 Department of Geology, Post-Graduate College of Science, Osmania University, Saifabad, Hyderabad-500 004, India
     

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The calc-alkaline complex of Chanduluru (CL) in the Prakasam alkaline province of Andhra Pradesh is composed of two distinct petrographic suites viz. a gabbro-diorite suite and a melasyenitegranite suite. The chief rock forming minerals of the complex are clinopyroxene, amphibole, biotite, plagioclase, K-feldspar and quartz; the accessory minerals include apatite, sphene, zircon, opaque oxide and garnet.

Major, trace and rare earth element variations in the two suites of rocks suggest two distinct petrogenetic series. The two suites are derived from two different parental magmas of varying composition and source. A mantle derived gabbroic magma has yielded gabbro-diorite suite by fractional crystalliiation. The underplating of the gabbroic magma has led to partial melting of the LREE-enriched arnphibolite crust to yield a melasyenitic magma, which on fractional crystallization has yielded melasyenitegranite suite. The complex is emplaced in a within-plate-collision tectonic environment.


Keywords

Igneous Petrology, Gabbro, Diorite, Syenite, Granite, Partial Melting, Fractional Crystallization, Chanduluru Complex, Prakasam Alkaline Province, Andhra Pradesh.
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  • Petrology of the Gabbro-Diorite-Syenite-Granite Complex of Chanduluru, Prakasam Alkaline Province, Andhra Pradesh, India

Abstract Views: 188  |  PDF Views: 2

Authors

V. Nagsai Sharma
Department of Geology, Post-Graduate College of Science, Osmania University, Saifabad, Hyderabad-500 004, India
J. Ratnakar
Department of Geology, Post-Graduate College of Science, Osmania University, Saifabad, Hyderabad-500 004, India

Abstract


The calc-alkaline complex of Chanduluru (CL) in the Prakasam alkaline province of Andhra Pradesh is composed of two distinct petrographic suites viz. a gabbro-diorite suite and a melasyenitegranite suite. The chief rock forming minerals of the complex are clinopyroxene, amphibole, biotite, plagioclase, K-feldspar and quartz; the accessory minerals include apatite, sphene, zircon, opaque oxide and garnet.

Major, trace and rare earth element variations in the two suites of rocks suggest two distinct petrogenetic series. The two suites are derived from two different parental magmas of varying composition and source. A mantle derived gabbroic magma has yielded gabbro-diorite suite by fractional crystalliiation. The underplating of the gabbroic magma has led to partial melting of the LREE-enriched arnphibolite crust to yield a melasyenitic magma, which on fractional crystallization has yielded melasyenitegranite suite. The complex is emplaced in a within-plate-collision tectonic environment.


Keywords


Igneous Petrology, Gabbro, Diorite, Syenite, Granite, Partial Melting, Fractional Crystallization, Chanduluru Complex, Prakasam Alkaline Province, Andhra Pradesh.