阿拉善地块北大山地区两类辉长岩的锆石U-Pb定年、Hf同位素及地球化学特征——对中亚造山带构造演化的启示
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摘要
作为中亚造山带的重要组成,阿拉善地块北缘已成为研究古亚洲洋构造演化历史的关键地区。本次工作对阿拉善地块北大山地区两类辉长岩进行LA-ICP-MS锆石U-Pb测年,获得成岩年龄分别为293±2Ma和267±2Ma,为早、中二叠世。早二叠世辉长岩为堆晶岩,呈亚碱性,拉斑玄武质,高Mg#值(64)、Eu显著正异常、极低的REE、富集大离子亲石元素(Ba、K、Sr),亏损高场强元素(Th、Nb、Ta、Hf、Zr),锆石的εHf(t)平均值为0.91,以上特征显示其岩浆源区为受俯冲板片混染或交代的岩石圈地幔,形成于俯冲相关的挤压环境;中二叠世辉长岩呈碱性、富集大离子亲石元素(Ba、K)和稀土元素,但Nb、Ta等高场强元素亏损不明显,锆石的εHf(t)平均值为3.5,显示其岩浆源区为受陆壳混染的亏损地幔,形成于大陆板内拉张环境。综合本文及前人研究成果,认为阿拉善地块北缘存在一条西起龙首山,东到狼山的晚古生代(328~262 Ma)超基性—基性岩浆带,其形成与古亚洲洋的俯冲—闭合—造山后伸展过程相关。在晚石炭世—早二叠世晚期,阿拉善地块北缘为大洋俯冲环境,到早二叠世晚期—中二叠世进入大陆板内拉张环境,限定了古亚洲洋在阿拉善地块北缘的最终闭合时代为早二叠世晚期—中二叠世。
As an important component of the Central Asian Orogenic Belt(CAOB),the Alxa Block has been a key area for studying the tectonic evolution history of the Paleo-Asian Ocean(PAO).This study carried out LA-ICP-MS zircon U-Pb dating for two types of gabbros from the Beidashan region in the Alxa Block,yielding two rock-forming ages of 293±2 Ma and 267±2 Ma(early and middle Permian).The early Permian gabbro(293±2(64),positive Eu anomaly,low rare earth elements(REE),enrichment of large ion lithophile elements(LILE;Ba,K,Sr),depletion of high field strength elements(HFSE;Th,Nb,Ta,Hf,Zr),and low positive(0.91).All of these characteristics indicate that the early-Permian gabbro derived from a lithospheric mantle metasomatized by slab-derived fluids or melt in an oceanic subduction tectonic setting.The middle Permian gabbro(267±2 Ma)is alkaline,enriched in LILE(Ba,K)and REE,butPermian gabbro derived from the depleted mantle with crustal contamination in a continental intraplate extensional setting.Combined with previous research,this study can conclude that one late Paleozoic(328~262Ma)ultramafic-mafic rock belt extending from Longshoushan in the west to the Langshan in the east occurs in the northern margin of Alxa block and formed in the subduction and closure of the PAO.The northern margin of Alxa Block was an oceanic subduction environment during late Carboniferous to late early-Permian,and transferred into a continental intraplate extensional environment during late earlyPermian to middle-Permian,which restricts that timing of the final closure of the PAO in the northern margin of Alxa Block was between late early-Permian and middle-Permian.
As an important component of the Central Asian Orogenic Belt(CAOB),the Alxa Block has been a key area for studying the tectonic evolution history of the Paleo-Asian Ocean(PAO).This study carried out LA-ICP-MS zircon U-Pb dating for two types of gabbros from the Beidashan region in the Alxa Block,yielding two rock-forming ages of 293±2 Ma and 267±2 Ma(early and middle Permian).The early Permian gabbro(293±2(64),positive Eu anomaly,low rare earth elements(REE),enrichment of large ion lithophile elements(LILE;Ba,K,Sr),depletion of high field strength elements(HFSE;Th,Nb,Ta,Hf,Zr),and low positive(0.91).All of these characteristics indicate that the early-Permian gabbro derived from a lithospheric mantle metasomatized by slab-derived fluids or melt in an oceanic subduction tectonic setting.The middle Permian gabbro(267±2 Ma)is alkaline,enriched in LILE(Ba,K)and REE,butPermian gabbro derived from the depleted mantle with crustal contamination in a continental intraplate extensional setting.Combined with previous research,this study can conclude that one late Paleozoic(328~262Ma)ultramafic-mafic rock belt extending from Longshoushan in the west to the Langshan in the east occurs in the northern margin of Alxa block and formed in the subduction and closure of the PAO.The northern margin of Alxa Block was an oceanic subduction environment during late Carboniferous to late early-Permian,and transferred into a continental intraplate extensional environment during late earlyPermian to middle-Permian,which restricts that timing of the final closure of the PAO in the northern margin of Alxa Block was between late early-Permian and middle-Permian.
引文
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