新疆磁海超大型铁矿区基性岩及其成矿背景指示

齐天骄; 薛春纪; 张招崇; 王银宏; 邵发志

doi:10.3799/dqkx.2012.139

Volume 37 Issue 6

Jun. 2012

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Article Navigation > Earth Science > 2012 > 37(6): 1315-1326

QI Tian-jiao, XUE Chun-ji, ZHANG Zhao-chong, WANG Yin-hong, SHAO Fa-zhi, 2012. Basic Igneous Rock in Cihai Giant Iron District, Hami, Xinjiang, and Its Indication to the Metallogenic Setting. Earth Science, 37(6): 1315-1326. doi: 10.3799/dqkx.2012.139

Citation:

QI Tian-jiao, XUE Chun-ji, ZHANG Zhao-chong, WANG Yin-hong, SHAO Fa-zhi, 2012. Basic Igneous Rock in Cihai Giant Iron District, Hami, Xinjiang, and Its Indication to the Metallogenic Setting. Earth Science, 37(6): 1315-1326. doi: 10.3799/dqkx.2012.139

Citation:

QI Tian-jiao, XUE Chun-ji, ZHANG Zhao-chong, WANG Yin-hong, SHAO Fa-zhi, 2012. Basic Igneous Rock in Cihai Giant Iron District, Hami, Xinjiang, and Its Indication to the Metallogenic Setting. Earth Science, 37(6): 1315-1326. doi: 10.3799/dqkx.2012.139

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Basic Igneous Rock in Cihai Giant Iron District, Hami, Xinjiang, and Its Indication to the Metallogenic Setting

doi: 10.3799/dqkx.2012.139

1.
State Key Laboratory of Geological Processes and Mineral Resources, China University Geosciences, Beijing 100083, China
2.
Yakuang Iron and Steel Company, Xinjiang Province, Hami 839126, China

Received Date: 2012-07-19
Available Online: 2021-11-09
Publish Date: 2012-06-15

Abstract

Abstract

The basic igneous rock in Cihai giant iron district has a close relationship with the iron mineralization which is the key to understanding of the larger scale of iron metallization and the metallogenic setting. The diabase is the main basic igneous rock in Cihai iron district,and the platy iron-vein group are hosted by the fault-fissures in diabase; the U-Pb dating of single-grained zircon from diabase yielded an average weighted ²⁰⁶Pb/²³⁸U age of 263.8±3.6 Ma (n＝11,MSWD=1.3)which is contemporary with that of the basic igneous rock in Permian Tarim basin,eastern Tianshan orogenic belt and Beishan tectonic-metallogenic belt. The trace elements chondrite-normalized patterns of basic igneous rock in Cihai iron district are relatively flat with Sr,Ba enriched and Nb lost lightly; the REE chondrite-normalized patterns are flat. The content of trace elements and magmatic nature of basic igneous rock in Cihai iron district are similar to that of the basic igneous rocks in Permian Tarim basin,eastern Tianshan orogenic belt and Beishan tectonic-metallogenic belt and they all belong to alkaline-calc-alkaline series with close genetic relationship; the basic igneous magma of Cihai district most possibly originated from asthenospheric mantle. The basic igneous rock in Cihai district is possibly a part of Tarim large igneous provinces formed by Permian mantle plum; and the large scale of iron mineralization are also formed in the setting of mantle plum which is a branch of mantle plum in Tarim basin as Beishan tectonic-metallogenic belt.
- basic igneous rock,
- Permian period,
- mantle plume setting,
- Cihai giant iron deposit,
- geochemistry,
- ore prospecting,
- ore deposits.

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References(84)

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Basic Igneous Rock in Cihai Giant Iron District, Hami, Xinjiang, and Its Indication to the Metallogenic Setting

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