首页|北准噶尔杜热一带晚古生代岩浆岩地球化学、年代学及地质意义

北准噶尔杜热一带晚古生代岩浆岩地球化学、年代学及地质意义

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北准噶尔杜热地区大面积被第四系覆盖,出露少量基性岩体,通过岩石化学、地球化学、同位素年代学,探讨杜热一带新发现辉长岩、闪长岩复合岩体成矿意义,分析该区找矿潜力.辉长岩微量元素显示富集Rb,K,La,Sr,Ti,亏损Th,Ta,Zr,Hf;闪长岩显示富集Rb,K,La,Sr,亏损Nb,Ta,辉长岩、闪长岩稀土元素显示岛弧火山岩特征.测试获得辉长岩和闪长岩形成年龄分别为(383.9±3.3)Ma和(386.2±3.8)Ma.
Geochemistry,Chronology and Geological Significance of Late Paleozoic Magmatic Rocks in Dure Area,Northern Junggar,Xinjiang
there are a few basic rocks in the Quaternary overlying area of the dure area,northern Junggar.In this paper,a new composite rock body of gabbro and diorite has been discovered in the dure area,based on petrochemistry,geo-chemistry and isotopic chronology,its significance for mineralization and prospecting potential are discussed.The gab-bro micronutrient show enrichment of Rb,K,La,Sr,TI and deficiency of Th,Ta,Zr,HF,while the diorite shows enrich-ment of Rb,K,La,SR and deficiency of NB,Ta,the rare earth elements of gabbro and diorite show the characteristics of island arc volcanic rocks.The ages of gabbro and diorite are(383.9±3.3)Ma and(386.2±3.8)Ma,respectively.

Northern JunggarZircon U-Pb datingDure

李咸阳、滕宇翔、郑飞、王哲

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新疆维吾尔自治区地质调查院,新疆乌鲁木齐 830000

北准噶尔 锆石U-Pb测年 杜热

中央引导地方科技资专项新疆维吾尔自治区自然科学基金

ZYYD2023A122022D01A288

2024

新疆地质
新疆维吾尔自治区地质学会

新疆地质

CSTPCD
影响因子:0.879
ISSN:1000-8845
年,卷(期):2024.42(1)
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