文章摘要
柏治安.秦岭岩群中斜长角闪岩的年代学、地球化学特征及其地质意义[J].地质与勘探,2020,56(2):372-386
秦岭岩群中斜长角闪岩的年代学、地球化学特征及其地质意义
Geochronology and geochemical characteristics of the amphibolites from the Qinling Group and their geological implications
投稿时间:2019-01-16  修订日期:2019-11-25
DOI:10.12134/j.dzykt.2020.02.012
中文关键词: 秦岭岩群 斜长角闪岩 锆石年代学 构造背景 构造归属
英文关键词: Qinling Group, amphibolites, zircon geochronology, tectonic setting, tectonic affinity
基金项目:国家自然科学基金(编号:41302155, 41562005, 41862003)和广西自然科学基金杰出青年基金(编号: 2018GXNSFFA281009)联合资助
作者单位E-mail
柏治安 广西隐伏金属矿产勘查重点实验室桂林理工大学广西桂林 广西壮族自治区二七四地质队广西北海 广西有色金属隐伏矿床勘查及材料开发协同创新中心广西桂林 shiyu_61@163.com 
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中文摘要:
      本文对秦岭岩群中的三个斜长角闪岩(变质沉积岩)样品进行了岩石学、锆石U-Pb年代学和岩石地球化学研究,限定了秦岭岩群的形成时代,讨论了秦岭岩群的构造背景及归属问题。锆石定年结果显示了971 Ma、1222 Ma和840 Ma三个最大沉积年龄。秦岭岩群是一个杂岩体,秦岭岩群中至少存在中元古代(较老组成部分)和新元古代早期(较新组成部分)的岩性单元。秦岭岩群变质沉积岩的锆石年龄峰主要集中在中元古代-新元古代早期,具有与扬子块体和华北块体明显不同的锆石年代学特征,秦岭岩群在中元古代-新元古代早期为独立发展的微陆块。结合秦岭岩群的年代学特征及前人的研究结果,秦岭岩群中的变质沉积岩应沉积于弧相关的构造环境。
英文摘要:
      This paper presents a study on petrology, zircon U-Pb dating and geochemistry of three amphibolites (meta-sedimentary rock) samples from the Qinling Group, which permits to constrain their formation ages, tectonic setting and tectonic affinity. Zircon dating results show three maximum depositional ages of 971 Ma, 1222 Ma and 840 Ma of this rock. The Qinling Group is considered to be a complex with units of the Mesoproterozoic (older components) and early Neoproterozoic (newer components). The age peaks of the meta-sedimentary rocks from the Qinling Group are mainly clustering at Mesoproterozoic to early Neoproterozoic, which are different from the Yangtze block and North China block. Research suggests that he Qinling Group formed in a microcontinent with distinct evolution during Mesoproterozoic to early Neoproterozoic. Combined with the geochronological characteristics and previous research, this study deems that the meta-sedimentary rocks in the Qinling Group deposited in a arc-related tectonic environment.
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