古特提斯演化的岩浆作用记录:来自桂东南印支期火山岩证据  

Magmatism Records of Palaeo-Tethyan Evolution:Evidence from Indosinian Volcanic Rocks in Southeastern Guangxi

作　　者：覃悦 蔡永丰[1,2] 刘军 刘希军[1,2] 周云 李政林[1,2] 杨栎娅 Qin Yue;Cai Yongfeng;Liu Jun;Liu Xijun;Zhou Yun;Li Zhenglin;Yang Liya(Guangxi Key Laboratory of Hidden Metallic Ore Deposits Exploration,Guilin University of Technology,Guilin 541004,China;Collaborative Innovation Center for Exploration of Nonferrous Metal Deposits and Efficient Utilization of Resources in Guangxi,Guilin University of Technology,Guilin 541004,China;Yantai Earthquake Monitoring Center Station,Shandong Earthquake Agency,Yantai 264009,China)

机构地区：[1]桂林理工大学广西隐伏金属矿产勘查重点实验室,广西桂林541004 [2]桂林理工大学有色金属矿产勘查与资源高效利用省部共建协同创新中心,广西桂林541004 [3]山东省地震局烟台地震监测中心站,山东烟台264009

出　　处：《地球科学》2024年第9期3140-3154,共15页Earth Science

基　　金：广西自然科学基金项目(No.2022GXNSFAA035620);国家自然科学基金项目(Nos.92055208,42372102);广西重点研发计划项目(No.桂科AB22035045).

摘　　要：为了探讨古特提斯构造演化是否在华南大陆西南缘保存有岩浆作用记录,本文对桂东南印支期火山岩开展了年代学和元素地球化学分析.研究结果表明,两个代表性英安斑岩样品分别给出了(245±2)Ma和(247±4)Ma的形成时代,表明桂东南发育早‒中三叠世火山作用.英安斑岩具有高钾、富铝、贫钛、贫镁的特征,表现出准铝质高钾钙碱性岩石的特征.样品总体富集Rb、Th、U,亏损Ti、Ba、P、Sr,Nb、Ta负异常明显.轻、重稀土分馏较明显,Eu具中等负异常.综合分析表明,英安斑岩主要来源于地壳物质的熔融,并经历了一定程度的分离结晶作用;桂东南与海南岛、金沙江、哀牢山一带的印支早期岩浆岩在岩石类型、地球化学特征、沉积序列和古生物化石方面均具有可对比性,暗示这些地区在印支早期可能经历了相似的构造演化事件,主要受控于古特提斯构造域,推测桂东南于早‒中三叠世进入同碰撞阶段.To determine the availability of the magmatism records of Palaeo-Tethyan evolution in the southeastern margin of the South China continent,detailed LA-ICP-MS zircon U-Pb geochronological and elemental geochemical analyses of the Indosinian volcanic rocks in the southeastern Guangxi have been carried out in this paper.Geochronological results show that two representative dacite porphyry samples yield zircon U-Pb ages of(245±2)Ma and(247±4)Ma,respectively,indicating that Early to Middle Triassic volcanism occurred in the southeastern Guangxi.Elemental geochemical results show that the dacite porphyry is characterized by high K_(2)O and Al_(2)O_(3) contents,and low TiO_(2) and MgO contents,belonging to the metaluminous high-K calc-alkaline series rocks.The samples show enrichment in Rb,Th,and U,and are characterized by negative Ba,Ti,Sr,P,and Nb-Ta anomalies.They also show obvious LREE and HREE fractionation,and have moderate negative Eu anomalies.The above data indicate that the dacite porphyry mainly originated from the melting of crustal materials,and fractional crystallization occurred during the process of magmatic evolution.Combined with regional geological data,it is suggested that the Indosinian magmatic rock assemblages,geochemical characteristics,sedimentary sequences,and paleontological fossils in the southeastern Guangxi are comparable to those in the Hainan Island and Jinshajiang-Ailaoshan regions,suggesting that these regions may have experienced similar tectonic events during the Indosinian Period,which were mainly controlled by the Palaeo-Tethyan tectonic domain during the Indosinian.The formation of the Indosinian dacite porphyry in southeastern Guangxi possibly represents a syn-collisional stage during the Early to Middle Triassic.

关 键 词：英安斑岩 锆石U⁃Pb年龄 地球化学 古特提斯 桂东南钦防地区 岩石学. 

分 类 号：P595[天文地球—地球化学] P597[天文地球—地质学]