锆石U-Pb年代学和地球化学对浙皖马鞍山高分异岩体成因的约束

张建芳; 汪隆武; 陈津华; 朱朝晖; 刘健; 章明圆

doi:10.3799/dqkx.2015.007

Volume 40 Issue 1

Jan. 2015

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Article Navigation > Earth Science > 2015 > 40(1): 98-114

Zhang Jianfang, Wang Longwu, Chen Jinhua, Zhu Chaohui, Liu Jian, Zhang Mingyuan, 2015. Genesis of Highly Fractionated Ma'anshan Rock in Zhejiang and Anhui Provinces Constrained by U-Pb Zircon Geochronology and Geochemistry. Earth Science, 40(1): 98-114. doi: 10.3799/dqkx.2015.007

Citation:

Zhang Jianfang, Wang Longwu, Chen Jinhua, Zhu Chaohui, Liu Jian, Zhang Mingyuan, 2015. Genesis of Highly Fractionated Ma'anshan Rock in Zhejiang and Anhui Provinces Constrained by U-Pb Zircon Geochronology and Geochemistry. Earth Science, 40(1): 98-114. doi: 10.3799/dqkx.2015.007

Citation:

Zhang Jianfang, Wang Longwu, Chen Jinhua, Zhu Chaohui, Liu Jian, Zhang Mingyuan, 2015. Genesis of Highly Fractionated Ma'anshan Rock in Zhejiang and Anhui Provinces Constrained by U-Pb Zircon Geochronology and Geochemistry. Earth Science, 40(1): 98-114. doi: 10.3799/dqkx.2015.007

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Genesis of Highly Fractionated Ma'anshan Rock in Zhejiang and Anhui Provinces Constrained by U-Pb Zircon Geochronology and Geochemistry

doi: 10.3799/dqkx.2015.007

Zhejiang Institute of Geological Survey, Hangzhou 311203, China

Received Date: 2014-05-01
Publish Date: 2015-01-15

Abstract

Abstract

To understand the genesis of Ma'anshan rock composed of early period pegmatite and megacryst porphyritic adamellite, medium period fine granite and late period granite porphyry dykes, intrusion epochs are confirmed using SHRIMP and LA-ICP-MS zircon U-Pb methods. The dating shows that the pegmatite porphyritic adamellite is 132.2±1.6 Ma (MSWD=1.9, n=11), the megacrysts porphyritic adamellite 127.7 ±1.2 Ma (MSWD=1.1, n=10), the fine-grained granite 128.3±1.1 Ma (MSWD=1.7, n=10) and the granite porphyry dykes 127.4±1.8 Ma (MSWD=0.77, n=11). Rock geochemistry shows that the rock from early to late has the characteristic of alkali series shoshonite series evolving to high potassium calc (during evolution), whereas the differentiation degree gradually increases. The porphyritic adamellites have the characteristics of high ΣREE content, obvious differentiation between light rare earth and heavy rare earth elements, with a strong negative Eu anomaly and weak rightward REE distribution patterns. It is enriched in elements of K, Th, U, Rb and weakly depleted in Ba, Sr, P, Nb, Ta, Ti. The fine-grained granite and granite porphyry dyke have the characteristics of lower ΣREE content, not obvious differentiation between light and heavy rare earth elements, with a strong negative Eu anomaly, and "V"-type REE distribution patterns. It is enriched in elements of K, Th, U, Rb, strongly depleted in Ba, Sr, P, Nb, Ti. Ma'anshan rock was formed by the function of partially molten magma emplacement successively crystallization differentiation and it is the product of intracontinental extension after the Early Cretaceous subduction orogeny in Northwest Zhejiang-South Anhui, with the characteristic of highly fractionated I-type granites.
- zircon U-Pb,
- geochemistry,
- petrogenesis,
- Ma'anshan rock,
- Zhejiang and Anhui border area

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References(105)

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Genesis of Highly Fractionated Ma'anshan Rock in Zhejiang and Anhui Provinces Constrained by U-Pb Zircon Geochronology and Geochemistry

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