冈底斯弧南缘侏罗纪岩浆弧地壳组成及俯冲和碰撞相关斑岩矿床成因联系——来自Nd同位素、ΔFMQ和Eu/Eu<sup>*</sup>填图的认识-岩石矿物学杂志-CSCIED科技核心评价数据库-手机版

冈底斯弧南缘侏罗纪岩浆弧地壳组成及俯冲和碰撞相关斑岩矿床成因联系——来自Nd同位素、ΔFMQ和Eu/Eu^*填图的认识

The crustal composition of Jurassic magmatic arc in the southern margin of the Gangdise arc and the genetic relationship between subduction and collision related porphyry deposits: Insights from Nd isotope, ΔFMQ, and Eu/Eu^* mapping

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DOI	10.20086/j.cnki.yskw.2024.0609
刊名	岩石矿物学杂志 Acta Petrologica et Mineralogica
年，卷(期)	2024, 43(6)
作者	全海辉，柴鹏*，朱雄飞，袁玲玲，苏崇斌，李龙星，罗关银，张万元，徐家益,
作者单位	1. 中国地质科学院地质研究所自然资源部深地科学与探测技术实验室, 北京 100094; 2. 墨江矿业有限责任公司, 云南墨江 654800; 3. 昌益矿业有限责任公司, 云南墨江 654800
摘要	侏罗纪岩浆弧位于冈底斯弧南缘,其中发育有侏罗纪与俯冲相关的Cu-Au和中新世与碰撞相关的Cu-Mo斑岩矿床。然而,目前对俯冲和碰撞相关的斑岩Cu矿床之间的成因联系知之甚少。本文以已发表的侏罗纪弧岩浆岩全岩主微量元素、Sm-Nd同位素和锆石微量元素数据为基础,在侏罗纪岩浆弧范围内进行了全岩Nd同位素、锆石ΔFMQ和Eu/Eu^值填图。填图结果显示,侏罗纪与俯冲相关的斑岩Cu-Au矿床主要发育区域,在侏罗纪时期具有高εNd(t)和年轻Nd模式年龄,表现出新生地壳特征,而中新世与碰撞相关的斑岩Cu-Mo矿床发育位置,在侏罗纪时期为新老地壳接触界面附近;侏罗纪斑岩Cu-Au矿床基本发育于在侏罗纪时期具有高ΔFMQ和Eu/Eu^值的岩浆区域,中新世斑岩Cu-Mo矿床发育区域的岩浆,在侏罗纪时期表现出高ΔFMQ、低Eu/Eu^值或低ΔFMQ、Eu/Eu^值的特征。这表明在侏罗纪时期,侏罗纪斑岩Cu-Au矿床所在区域的岩浆,相较于中新世斑岩Cu-Mo矿床发育区域的岩浆,具有更高的氧逸度和含水量。富水和氧化的岩浆通过抑制深部岩浆的早期硫化物饱和,为侏罗纪斑岩Cu-Au矿床的发育提供了充足的S和成矿金属。相对而言,中新世斑岩Cu-Mo矿床发育区域岩浆可能由于古老地壳组分混入而未达到抑制深部岩浆早期硫化物饱和条件,触发了早期硫化物饱,导致大量含Cu下地壳堆积形成,抑制了其在侏罗纪成矿。印度-欧亚大陆碰撞导致热软流圈熔体底侵,触发了含Cu下地壳堆晶重熔,为中新世斑岩Cu-Mo矿床的形成提供了有利的金属来源。
Abstract	The Jurassic magmatic arc is located on the southern margin of the Gondwanan arc, in which Jurassic subduction-related Cu-Au and Miocene collision-related Cu-Mo porphyry deposits are developed. However, little is known about the diagenetic links between subduction- and collision-related porphyry Cu deposits. In this paper, Nd isotope, ΔFMQ and Eu/Eu^* value mapping has been carried out within the Jurassic magmatic arc, based on published whole-rock major and trace elements, Sm-Nd isotope and zircon trace elements data. The mapping results show that the main development area of Jurassic subduction-related porphyry Cu-Au deposits has high εNd(t) and young Nd mode ages during the Jurassic period, which exhibit juvenile crustal features, while the development location of Miocene collision-related porphyry Cu-Mo deposits is near the interface of the crustal contact between the old and juvenile crust during the Jurassic period. Jurassic porphyry Cu-Au deposits were basically developed in areas with high ΔFMQ and Eu/Eu^* value magmas during the Jurassic period, and Miocene porphyry Cu-Mo deposits were developed in areas that exhibit either areas of high ΔFMQ and low Eu/Eu^* value or areas of low ΔFMQ and Eu/Eu^* values during the Jurassic period. This indicates that during the Jurassic period, the magma in the area where the Jurassic porphyry Cu-Au deposits are located had higher oxygen fugacity and water content compared to the magma in the area where the Miocene porphyry Cu-Mo deposits were developed. Water-rich and oxidised magmas provided sufficient S and metallogenic metals for the development of Jurassic porphyry Cu-Au deposits by inhibiting early sulphide saturation of deeper magmas. Comparatively, the magma of the Miocene porphyry Cu-Mo development region may have failed to reach conditions that inhibited early sulphide saturation in the deeper magma due to the mixing of ancient crustal components, which triggered early sulphide saturation, leading to the formation of large amounts of Cu-bearing lower crustal accretion and inhibiting its mineralisation in the Jurassic. The Indian-Eurasian collision resulted in the bottom intrusion of thermochondritic melts, which triggered the remelting of Cu-bearing lower crustal heap crystals, providing a favourable source of metals for the formation of the Miocene porphyry Cu-Mo deposits.
关键词	斑岩铜矿；Nd同位素填图；锆石ΔFMQ填图；锆石Eu/Eu^*填图；侏罗纪岩浆弧
KeyWord	porphyry Cu deposits; Nd isotope mapping; zircon ΔFMQ mapping; zircon Eu/Eu^* mapping; Jurassic magmatic arc
基金项目
页码	1513-1530

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全海辉，柴鹏*，朱雄飞，袁玲玲，苏崇斌，李龙星，罗关银，张万元，徐家益. 冈底斯弧南缘侏罗纪岩浆弧地壳组成及俯冲和碰撞相关斑岩矿床成因联系——来自Nd同位素、ΔFMQ和Eu/Eu^*填图的认识 [J]. 岩石矿物学杂志. 2024; 43; (6). 1513 - 1530.

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