[an error occurred while processing this directive] [an error occurred while processing this directive]
[an error occurred while processing this directive]Composition of Gold and Other Elements in the Mesozoic Magmatic Rocks of the Jiaodong Peninsula and Their Implications for Gold Mineralization
Received date: 2024-05-30
Revised date: 2024-07-29
Online published: 2024-09-19
The Jiaodong Peninsula is the largest gold-producing region in China,however,the sources of its substantial gold reserves remains uncertain.Analyzing the trace elements in pre-mineralization Late Jurassic Linglong-type plutons (Linglong,Kunyushan),Early Cretaceous Guojialing-type plutons (Guojialing,Congjia),syn- to post-mineralization Early Cretaceous Weideshan-type plutons,and the mafic dioritic enclaves within the latter two plutons reveals that these formations generally exhibit lower concentrations of elements such as Cu,Au,Ag,Sb,and As compared to the average values of the continental crust.Specifically,the gold content is typically below 0.5×10-9,aligning with prior test results and suggesting a depletion process of elements such as gold during magmatic evolution.Furthermore,a significant positive correlation is observed between the Cu/Ag ratio and Cu content in both Linglong-type and Weideshan-type samples.In Guojialing-type plutons and their enclaves,a positive correlation between the Cu/Ag ratio and Au content has been observed.This relationship suggests that during magma evolution,monosulfide solid solution continuously separates from the magma.Consequently,Mesozoic magmatic rocks exhibit lower Cu/Ag ratios and reduced metal content.The accumulation of these sulfides in the middle to lower crust forms an enriched source layer of gold and other elements,thereby providing ore-forming materials essential for gold mineralization in the Jiaodong region.The study also suggests that the separation of monosulfide solid solutions during magma evolution may be a common process,which could also explain why the continental crust is depleted in copper and other elements compared to the mantle.
Leilei DONG , Xin BAI , Mingchun SONG . Composition of Gold and Other Elements in the Mesozoic Magmatic Rocks of the Jiaodong Peninsula and Their Implications for Gold Mineralization[J]. Gold Science and Technology, 2024 , 32(5) : 768 -780 . DOI: 10.11872/j.issn.1005-518.2024.05.156
http://www.goldsci.ac.cn/article/2024/1005-2518/1005-2518-2024-32-5-768.shtml
感谢山东省物化探勘查院王润生、于林松、高晓丰和山东省地质矿产勘查开发局第六地质大队王斌等协助野外考察和采样。审稿专家对本文提出了宝贵意见和建议,谨此致谢!
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
陈玉民,曾庆栋,孙之夫,等,2019.胶东金地球化学背景研究[J].黄金科学技术,27(6):791-801.
|
|
高天山,陈江峰,谢智,等,2004.苏鲁超高压变质带中三叠纪石岛杂岩体的地球化学研究[J].岩石学报,20(5):1025-1038.
|
|
郭敬辉,陈福坤,张晓曼,等,2005.苏鲁超高压带北部中生代岩浆侵入活动与同碰撞—碰撞后构造过程:锆石 U-Pb 年代学[J].岩石学报,21(4):1281-1301.
|
|
刘平华,刘福来,王舫,2015.胶北地体多期变质事件的P-T-t轨迹及其对胶—辽—吉带形成与演化的制约[J].岩石学报,31(10):2889-2941.
|
|
陆丽娜,范宏瑞,胡芳芳,等,2011.胶西北郭家岭花岗闪长岩侵位深度:来自角闪石温压计和流体包裹体的证据[J].岩石学报,27(5):1521-1532.
|
|
万渝生,董春艳,任鹏,等,2017.华北克拉通太古宙TTG岩石的时空分布、组成特征及形成演化:综述[J].岩石学报,33(5):1405-1419.
|
|
杨进辉,朱美妃,刘伟,等,2003.胶东地区郭家岭花岗闪长岩的地球化学特征及成因[J].岩石学报,19(4):692-700.
|
|
曾令森,陈晶,陈振宇,等,2007.山东石岛花岗岩复合岩体的侵位深度与苏鲁超高压变质岩的快速折返机制及动力学效应[J].岩石学报,23(12):3171-3179.
|
|
张岳桥,李金良,张田,等,2007.胶东半岛牟平—即墨断裂带晚中生代运动学转换历史[J].地质论评,53(3):289-300.
|
|
朱光,刘程,顾承串,等,2018.郯庐断裂带晚中生代演化对西太平洋俯冲历史的指示[J].中国科学:地球科学,48(4):415-435.
|
/
| 〈 |
|
〉 |