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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:

第44卷

期数:

2022年第03期

页码:

499-512

栏目:

基础地质与矿产地质

出版日期:

2022-05-15

文章信息/Info

Title:

Discovery of High-Mg Diorites in Nabire Area, Indonesia and Its Implications

文章编号:

1672-6561(2022)03-0499-14

作者:

张 波¹; 2; 徐英豪²; 王国栋³; 4; 崔晓亮⁵; 李增胜⁶; 7; 苏尚国^2*; 陈学根²

(1. 中国地质调查局发展研究中心,北京 100037; 2. 中国地质大学(北京)地球科学与资源学院,北京 100083; 3. 临沂大学 资源环境学院,山东 临沂 276005; 4. 临沂大学 山东省水土保持与环境保育重点实验室,山东 临沂 276005; 5. 河北工程大学 水利水电学院,河北 邯郸 056038; 6. 山东省地质科学研究院 山东省金属矿产成矿地质过程与资源利用重点实验室,山东 济南 250013; 7. 自然资源部金矿成矿过程与资源利用重点实验室,山东 济南 250013)

Author(s):

ZHANG Bo¹; 2;  XU Ying-hao²;  WANG Guo-dong³; 4;  CUI Xiao-liang⁵;  LI Zeng-sheng⁶; 7;  SU Shang-guo^2*;  CHEN Xue-gen²

(1. Development and Research Center, China Geological Survey, Beijing 100037, China; 2. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China; 3. School of Resources and Environment, Linyi University, Linyi 276005, Shandong, China; 4. Shandong Provincial Key Laboratory of Water and Soil Conservation and Environmental Protection, Linyi University, Linyi 276005, Shandong, China; 5. School of Water Conservancy and Hydroelectric Power, Hebei University of Engineering, Handan 056038, Hebei, China; 6. Shandong Provincial Key Laboratory of Metallogenic Geological Processes and Resource Utilization, Shandong Institute of Geological Sciences, Jinan 250013, Shandong, China; 7. Key Laboratory of Gold Mineralization Processes and Resource Utilization of Ministry of Natural Resources, Jinan 250013, Shandong, China)

关键词:

高镁闪长岩;  地球化学;  岩石成因;  铜金矿床;  构造环境;  板块俯冲;  新几内亚中央造山带

Keywords:

high-Mg diorite;  geochemistry;  petrogenesis;  Cu-Au deposit;  tectonic setting;  plate subduction;  Central Orogenic Belt of New Guinea

分类号:

P57; P59; P581

DOI:

10.19814/j.jese.2022.04042

文献标志码:

A

摘要:

新几内亚中央造山带是世界上最年轻的造山带,也是世界上最重要的斑岩型铜金成矿带。位于新几内亚中央造山带中部偏西北的印度尼西亚纳比雷地区发现有一套高镁闪长岩岩体发育,为详细研究与大洋俯冲有关的岩浆过程和成矿环境提供了良好的记录。通过野外观察以及岩石学和地球化学特征研究发现:该高镁闪长岩以细粒角闪石和斜长石为主,未发现橄榄石捕虏体或捕虏晶; 岩石具有较高的MgO含量(质量分数,下同)(4.51%～10.88%)、Yb含量((1.16～2.69)×10^-6)及Y含量((11.68～25.09)×10^-6),高的Mg^#值(50.07～72.50),富集大离子亲石元素,亏损高场强元素,相对低的Sr/Y和La/Yb值; 结合较为一致的Nb/La、U/Nb、Th/La和U/Th值,表明其可能是由俯冲沉积物熔体与上覆地幔橄榄岩相互作用,并经历分离结晶作用演化而来,这一过程伴随了大量H₂O和流体的释放,增加了氧逸度; 高镁安山岩/闪长岩形成环境与斑岩型铜金矿床类似,与斑岩型铜金矿床具有紧密的亲和关系,是大型斑岩型矿床的找矿标志,而纳比雷地区高镁闪长岩已发现具有铜金矿化的发育,表明该地区具有寻找大型铜金矿床的潜力。

Abstract:

The Central Orogenic Belt of New Guinea is the youngest orogenic belt, and is also the most important porphyry-type Cu-Au metallogenic belt around the world. A set of high-Mg diorites have been found in Nabire area, Indonesia, which is located in the central-northwestern part of Central Orogenic Belt of New Guinea. They provide favorable records for the detailed study of the magmatic process and metallogenic environment related to ocean subduction. As revealed by field observations and the study of petrological and geochemical characteristics, these diorites mainly include fine-grained amphiboles and plagioclases, with no visible olivine xenoliths or xenocrysts. These rocks have high contents of MgO(4.51%-10.88%), Yb((1.16-2.69)×10^-6), and Y((11.68-25.09)×10^-6), and high Mg^#(50.07-72.50). Moreover, they are enriched in LILEs and depleted in HFSEs, and have low Sr/Y and La/Yb ratios. Combined with relatively consistent Nb/La, U/Nb, Th/La, and U/Th ratios, the high-Mg diorites may have evolved from the interactions between subduction sediment melt and overlying mantle peridotite, as well as fractional crystallization. This evolution was accompanied by the release of large amounts of H₂O and fluids, leading to the increase of oxygen fugacity. Relevant studies show that high-Mg andesites/diorites have a similar formation environment to that of porphyry-type Cu-Au deposits and a close affinity with porphyry-type Cu-Au deposits, and thus serve as a prospecting indicator of large porphyry deposits. The Cu-Au mineralization has occurred in high-Mg diorites of Nabire area, indicating that this area has the potential for the prospecting of large Cu-Au deposits.

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备注/Memo

备注/Memo:

收稿日期:2022-04-28; 修回日期:2022-05-08
基金项目:国家重点研发计划项目(2016YFE0202200); 山东省自然科学基金项目(ZR2018BD012)
作者简介:张 波(1986-),男,贵州遵义人,中国地质调查局发展研究中心工程师,理学博士,博士后,E-mail:zbotdw@163.com。
*通讯作者:苏尚国(1965-),男,湖南宁乡人,教授,博士研究生导师,理学博士,E-mail:susg@cugb.edu.cn。

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