Nature and(in-)coherent metamorphic evolution of subducted continental crust in the Neoproterozoic accretionary collage of SW Mongolia  

作　　者：Sergei Skuzovatov 

机构地区：[1]Vinogradov Institute of Geochemistry SB RAS,Favorskogo str.1A,Irkutsk 664033,Russia

出　　处：《Geoscience Frontiers》2021年第3期78-103,共26页地学前缘（英文版）

基　　金：performed within the framework of the IGC State Assignment Project No.0350-2016-0028;Ministry of Science and Technology of Taiwan(MOST 106-2811-M-001-035)during postdoctoral research of SYuS at Institute of Earth Science(Academia Sinica,Taipei,Taiwan);further supported by the Foundation of Russian Federation President(Grant No.MK-67.2020.5)。

摘　　要：In continental subduction complexes minor volumes of high-pressure mafic rocks(eclogites)often co-exist with much more abundant felsic(granitic)and metasedimentary rocks,which are vital for resolving the origin and metamorphic evolution of subducted continental crust.In SW Mongolia,the Alag Khadny eclogite-bearing accretionary complex(AKC)is assumed to represent either a remnant of oceanic slab,or a continental margin,subducted in the Early Cambrian.Here we present geochronological,geochemical and petrological evidence of subduction records for the three major types of lithologies that host mafic eclogites,including Mesoproterozoic and Neoproterozoic granitic basement and overlying Neoproterozoic continental-margin sediments.Variably deformed,ferroan and peraluminous metagranitoids compose a major part of AKC and are interlayered with eclogites in its southern and eastern margins.They have geochemical features of post-collisional/intraplate high-K calc-alkaline granites.LA-ICP-MS U-Pb zircon geochronology of three distinct metagranite samples show uniform protolith crystallization ages of ca.0.96 Ga and uncertain re-crystallization in the Late Neoproterozoic or Early Paleozoic metamorphic event,whereas abundant zircon inheritance indicates older,Mesoproterozoic to Paleoproterozoic crustal substrate during granite generation.The existence of Mesoproterozoic crust is highlighted by finding of distinct metagranitoids with the U-Pb zircon crystallization age of ca.1.6 Ga.Hafnium isotope signatures(T_(DM)^(C)2.88-1.85 Ga)of zircons from all lithologies preserved the evidence of reworked Neoarchean to Paleoproterozoic crust,similar to that of the Baidrag block(southern Mongolia),for both Mesoproterozoic and Neoproterozoic rocks.Regardless of the specific lithology,the rocks display indicators of high-pressure metamorphic re-equilibration,including garnet(X_(Ca)up to 0.65)+epidote+phengite(Si p.f.u.up to 3.56)±rutile assemblage in metagranitoids,garnet+phengite(Si p.f.u.up to 3.42)in quartz-rich semi-pelites and garnet

关 键 词：Central Asian Orogenic Belt SW Mongolia SUBDUCTION Metasedimentary rocks Orthogneisses Trace elements Zircon U-Pb age Hf isotopes 

分 类 号：P588.3[天文地球—岩石学] P542[天文地球—地质学]