首页> 外文期刊>Journal of Asian earth sciences >Mesoproterozoic island arc magmatism along the south-eastern margin of the Indian Plate: Evidence from geochemistry and zircon U-Pb ages of mafic plutonic complexes
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Mesoproterozoic island arc magmatism along the south-eastern margin of the Indian Plate: Evidence from geochemistry and zircon U-Pb ages of mafic plutonic complexes

机译:印度板块东南缘的中元古代岛弧岩浆作用:镁铁质深部复合体的地球化学和锆石U-Pb年龄的证据

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摘要

The Prakasam Igneous Province within the Nellore Schist Belt (NSB) preserves important imprints of mafic magmatism along the south-eastern margin of the Indian plate, Here we report petrology, geochemistry and zircon U-Pb age data from three gabbro plutons namely Purimetla, Kanigiri and P C Palle which intruded into the high grade rocks of the region. LA-ICP-MS U-Pb data on zircons from the three plutons reveal prominent late Mesoproterozoic ages of 1334 +/- 15 Ma, 1338 +/- 27 Ma and 1251.2 +/- 9.4 Ma. The cumulative (207)pb/Pb-206 mean age of 1315 +/- 11 Ma is interpreted to represent the timing of mafic magmatism in the Prakasam Igneous Province. These rocks show adcumulus to mesocumulus and poikilitic textures indicating fractional crystallization of plagioclase and clinopyroxenes in the Purimetla pluton whereas the Kanigiri and P C Palle intrusions possess hornblende and biotite suggesting the role of water during partial melting. The rocks show LREE enrichment (Sigma LREE/Sigma HREE = 2.2-15.0), marked Eu-anomalies (Eu/Eu* = 0.8-2.2) and fractionated patterns (La-N/Yb-N = 3-79). Primitive mantle normalised trace element spider diagrams indicate subduction modified arc signatures with LILE enrichment and depletion of Nb, Ti and Zr relative to Th and La. Tectonic discrimination diagrams show arc magmatic affinities for the three gabbro plutons consistent with subduction zone setting. We propose a tectonic model involving intra oceanic island arc accretion during late Mesoproterozoic along the eastern margin of the Indian continent. (C) 2016 Elsevier Ltd. All rights reserved.
机译:Nellore Schist带(NSB)内的Prakasam火成岩省保留了印度板块东南缘的镁铁质岩浆作用的重要印记。在这里,我们报告了来自三个辉长岩体Purimetla,Kanigiri的岩石学,地球化学和锆石U-Pb年龄数据和PC Palle闯入该地区的高级岩石。来自三个小行星的锆石的LA-ICP-MS U-Pb数据显示,中元古代的晚期年龄为1334 +/- 15 Ma,1338 +/- 27 Ma和1251.2 +/- 9.4 Ma。累积的(207)pb / Pb-206平均年龄为1315 +/- 11 Ma,被解释为代表了Prakasam火成岩省的镁铁质岩浆作用时期。这些岩石显示出丘陵至中丘陵和中质岩质地,表明斜长石和斜辉石在Purimetla岩体中有部分结晶,而Kanigiri和P C Palle侵入体具有角闪石和黑云母,表明水在部分融化过程中发挥了作用。岩石显示出LREE富集(Sigma LREE / Sigma HREE = 2.2-15.0),明显的Eu异常(Eu / Eu * = 0.8-2.2)和分度模式(La-N / Yb-N = 3-79)。原始地幔归一化微量元素蜘蛛图表明,相对于Th和La,LILE富集和耗尽的Nb,Ti和Zr具有俯冲作用的俯冲修饰弧特征。构造判别图显示了与俯冲带设定一致的三种辉长岩体的弧岩浆亲和力。我们提出了一个构造模型,涉及沿印度大陆东部边缘的中元古代晚期的大洋内岛弧增生。 (C)2016 Elsevier Ltd.保留所有权利。

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