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Petrographic and SHRIMP Studies of Zircons from the Caledonian Xiongdian Eclogite, Northwestern Dabie Mountains
Author(s) -
Ping JIAN,
Dunyi LIU,
Weiran YANG,
WILLIAMS I.S.
Publication year - 2000
Publication title -
acta geologica sinica ‐ english edition
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.444
H-Index - 61
eISSN - 1755-6724
pISSN - 1000-9515
DOI - 10.1111/j.1755-6724.2000.tb00492.x
Subject(s) - eclogite , metamorphic rock , geology , metamorphism , petrography , zircon , geochemistry , shrimp , radiogenic nuclide , metamorphic facies , pseudomorph , texture (cosmology) , mineralogy , tectonics , facies , subduction , paleontology , quartz , mantle (geology) , structural basin , artificial intelligence , fishery , biology , computer science , image (mathematics)
The Xiongdian eclogite occurring in the Sujiahe tectonic mélange zone at Luoshan County, Henan Province, in the western Dabie Mountains, is typical high‐pressure (HP)‐ultrahigh‐pressure (UHP) and medium‐temperature eclogite. The occurrence, internal texture and surface characteristics of zircons in eclogite were studied rather systematically petrographically combined with the cathodoluminescence (CL) and scanning electron microscope (SEM) methods. Zircons are mainly hosted in garnet and other metamorphic minerals with sharp boundaries, have a multifaceted morphology and are homogeneous or exhibit a metamorphic growth texture in the interior, thus indicating that they are the product of metamorphism. SHRIMP analyses give zircon 206 Pb/ 238 U ages of 335 to 424 Ma and show a certain degree of radiogenic Pb loss; therefore it may be inferred that the age of 424±5 Ma represents the minimum age of a HP‐UHP metamorphic age. From the above analyses coupled with previous Sm‐Nd, 40 Ar‐ 39 Ar, U‐Pb and 207 Pb/ 206 Pb age data, it is suggested that the peak metamorphic age of the Xiongdian eclogite should be between 424 and 480 Ma. This study further validate the view of the existence of a Caledonian HP‐UHP metamorphic event in the western Dabie Mountains.