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中国南方鄂东矿田与矿化及无矿花岗岩类中磷灰石和锆石的主量、微量元素及U-Pb年龄

Major, trace and rare earth elements of apatite and zircon U-Pb ages of ore-associated and barren granitoids from the Edong ore district, South China.

作者信息

Duan Deng-Fei, Jiang Shao-Yong

机构信息

State Key Laboratory of Geological Processes and Mineral Resources, Collaborative Innovation Centre for Exploration of Strategic Mineral Resources, Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, PR China.

出版信息

Data Brief. 2018 Sep 1;20:1587-1601. doi: 10.1016/j.dib.2018.08.154. eCollection 2018 Oct.

DOI:10.1016/j.dib.2018.08.154
PMID:30258964
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC6153191/
Abstract

The data in this article contains major, trace and rare earth element concentrations of apatite, and statistic analysis of apatite morphology in the granitoid rocks from the Edong ore district, South China, together with zircon U-Pb dating results for these rocks. Both the ore-associated and barren granitoids yield similar ages, including quartz diorite in the Fuzishan Cu-Au skarn deposit (138.6 ± 2.9 Ma), quartz monzodiorite in the Niutoushan Cu skarn deposit (137.8 ± 1.8 Ma), quartz diorite in the Ouyangshan Cu skarn deposit (138.4 ± 1.2 Ma), Liujiawan quartz monzodiorite (135.0 ± 2.4 Ma), and Bengqiaodi quartz monzodiorite porphyry (138.7 ± 1.1 Ma). Apatite occurs in all the minerals for each rock sample, and a detailed petrographic analysis shows the majority of them are early formed mineral phase. The F, Cl, SO contents in apatite are different, those in ore-associated rocks show higher values than barren ones. Li, Ni, Co, V contents are also higher in apatites from the ore-associated rocks than in barren rocks. Apatite (La/Sm) and (Yb/Sm) ratio show a positive correlation for ore-associated rocks but a negative correlation for barren rocks.

摘要

本文数据包含了鄂东南矿田花岗岩类岩石中磷灰石的主量、微量和稀土元素含量，磷灰石形态的统计分析结果，以及这些岩石的锆石U-Pb定年结果。与矿化有关的花岗岩类和无矿花岗岩类具有相似的年龄，包括伏牛山铜-金矽卡岩矿床中的石英闪长岩（138.6±2.9Ma）、牛头山铜矽卡岩矿床中的石英二长闪长岩（137.8±1.8Ma）、欧阳山铜矽卡岩矿床中的石英闪长岩（138.4±1.2Ma）、刘家湾石英二长闪长岩（135.0±2.4Ma）和崩桥底石英二长闪长斑岩（138.7±1.1Ma）。每个岩石样品的所有矿物中均有磷灰石产出，详细的岩相分析表明，它们大多数为早期形成的矿物相。磷灰石中的F、Cl、SO含量不同，与矿化有关岩石中的含量高于无矿岩石。与矿化有关岩石中磷灰石的Li、Ni、Co、V含量也高于无矿岩石。磷灰石的(La/Sm)和(Yb/Sm)比值在与矿化有关岩石中呈正相关，而在无矿岩石中呈负相关。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/55021639d48c/gr25.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/04d3393231e2/gr8.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/262676dbc886/gr9.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/4d6d499c0351/gr10.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/0516a4e80a8c/gr11.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/cd6db63b24b4/gr12.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/d209bd18f032/gr21.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/de1619045987/gr22.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/600260126e4e/gr23.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/f4126e07260a/gr1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/b175f4ed7df5/gr2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/23b73ef7d19f/gr3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/df298d5fb78d/gr4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/8a4cc5305eb5/gr5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/25146cdebd2f/gr6.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/48ce4063ba66/gr7.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/04d3393231e2/gr8.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/262676dbc886/gr9.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/4d6d499c0351/gr10.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/0516a4e80a8c/gr11.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/cd6db63b24b4/gr12.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/9b24c68699f6/gr13.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/eadef1e78445/gr14.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/f8a71c5d9a27/gr15.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/acc0441dd2cc/gr16.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/96205c72940f/gr17.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/7f1b9c9dad63/gr18.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/4b10ef518ecd/gr19.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/6368532f4bcf/gr20.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/d209bd18f032/gr21.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/de1619045987/gr22.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/600260126e4e/gr23.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ce62/6153191/55021639d48c/gr25.jpg

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