| 叶伟,陈超,朱颖,孔德才,刘治成,郭宇衡,龙波,郑娟.四川同德石墨矿床地球化学特征及原岩恢复[J].矿产勘查,2024,15(2):199-211 |
| 四川同德石墨矿床地球化学特征及原岩恢复 |
| Geochemical characteristics and protolith recovery of Tongde graphite deposit，Sichuan Province |
| 投稿时间：2022-05-02 修订日期：2022-06-26 |
| DOI：10.20008/j.kckc.202402003 |
| 中文关键词: 石墨 矿床地球化学 原岩恢复 同德 四川 |
| 英文关键词: graphite geochemical characteristics protolith restoration Tongde Sichuan Province |
| 基金项目:本文受四川省政府性投资地质勘查项目“四川省攀枝花市仁和区同德石墨矿普查”（DZ202104）和四川省自然资源科研项目“四川省晶质石墨成矿条件及分布规律研究”（kj-2021-10）联合资助。 |
| 作者 | 单位 | 邮编 | | 叶伟 | 四川省第四地质大队,四川 成都 611130 | 611130 | | 陈超* | 四川省第四地质大队,四川 成都 611130
四川省战略矿产资源勘查利用研究院,四川 成都 611130 | 611130 | | 朱颖 | 四川省第四地质大队,四川 成都 611130 | 611130 | | 孔德才 | 四川省第四地质大队,四川 成都 611130
四川省战略矿产资源勘查利用研究院,四川 成都 611130 | 611130 | | 刘治成 | 四川省国土科学技术研究院,四川 成都 610045 | 610045 | | 郭宇衡 | 四川省国土科学技术研究院,四川 成都 610045 | 610045 | | 龙波 | 四川省第四地质大队,四川 成都 611130
四川省战略矿产资源勘查利用研究院,四川 成都 611130 | 611130 | | 郑娟 | 四川省第四地质大队,四川 成都 611130 | 611130 |
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| 中文摘要: |
| 四川同德石墨矿床发现较早，矿床规模已达大型，但对其岩石地球化学和变质岩原岩恢复等方面的研究相对匮乏。本文通过对该矿床的全岩地球化学和碳同位素分析，探讨其地球化学特征和成岩成矿环境。分析结果表明，矿石SiO2为55.65%～61.68%，SiO2/Al2O3比值为4.59～5.42，Ni/Co平均比值8.73，富集Ba、Rb、Sr等大离子亲石元素，Nb、Zr、Hf、Th、U等高场强含量高。矿石ΣREE为149×10-6～195×10-6，轻稀土较为富集，具有弱的Ce负异常和Eu负异常，代表了极度贫氧—厌氧的海相沉积环境，矿石的原岩主要来源于陆源碎屑物质。稳定同位素结果显示石墨矿中碳同位素δ13CV-PDB值为-25.0‰~-23.5‰，表明其成矿碳质来源于有机物。综合野外地质调查认识和全岩地球化学原岩恢复结果，推测同德石墨矿床含矿片岩的原岩为一套含碳质黏土质杂砂岩沉积建造。 |
| 英文摘要: |
| The Tongde graphite deposit in Sichuan Province was discovered earlier and has reached a large scale. However， the studies on its rock geochemistry and proto-rock restoration of metamorphic rocks are relatively scarce. In this paper， the geochemical characteristics and diagenetic and metallogenic environment of the deposit are discussed through the analysis of whole rock geochemistry and carbon isotope. The analysis results show that SiO2 ranges from 55.65% to 61.68%， the ratio of SiO2/Al2O3 ranges from 4.59 to 5.42， and the average ratio of Ni/Co is 8.73. The ore is enriched with large ionic lithophile elements such as Ba， Rb and Sr， and has high field strength contents such as Nb， Zr， Hf， Th and U. The ΣREE of the ore is 149×10-6 ~ 195×10-6， and the light rare earth is relatively enriched with weak Ce and Eu negative anomalies， which represents an extremely oxygen-poor and anaerobic Marine sedimentary environment. The primary rock of the ore is mainly derived from terrigenous detritus. The stable isotope results show that the δ13CV-PDB values of the graphite ore are -25.0‰~-23.5‰， which indicates that the ore-forming carbon comes from organic matter. Based on the results of field geological investigation and whole rock geochemical protolith restoration， it is inferred that the protolith of the Tongde graphite deposit is composed of a set of carbonaceous clay sandstones. |
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