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SHRIMP U‐Pb Dating of Zircons of a Dark Eclogite and a Garnet‐bearing Gneissic Granitic Rock from Bixiling, Eastern Dabie Area, Anhui Province: Isotope Chronological Evidence of Neoproterozoic UHP Metamorphism
Author(s) -
Yuqi CHENG,
Dunyi LIU,
WILLIAMS I.S.,
Ping JIAN,
Yuxun ZHUANG,
Tianshan GAO
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.tb00491.x
Subject(s) - geology , eclogite , metamorphism , zircon , geochemistry , omphacite , metamorphic rock , coesite , metamorphic facies , protolith , feldspar , quartz , petrology , facies , subduction , geomorphology , paleontology , tectonics , structural basin
The paper reports SHRIMP U‐Pb zircon data of a dark eclogite and a post‐eclogite garnet‐bearing gneissic granitic rock from the Bixiling area, Yuexi County, Anhui Province, in the eastern Dabie Mountains. The eclogite, which is metamorphosed basic tuff, contains very scarce zircons in omphacite or garnet, but more zircons in quartz. They usually exhibit a double‐layered texture, as shown clearly in cathodoluminescence images. Their inner main parts give a 206 Pb/ 238 U age of 757±7 Ma, representing the approximate age of the high‐pressure (HP)‐ ultrahigh‐pressure (UHP) metamorphic event during which the eclogite was formed. The outer peripheral parts of the zircons, which have been modified by late‐stage fluids, give an age of 223±3 Ma. The granitic rock contains more zircons of anatectic origin found mostly in feldspar and quartz and usually also showing a similar composite texture. The inner main parts of the anatectic zircons with oscillatory zoning give a 206 Pb/ 238 U age of 727±15 Ma for the approximate age of the emplacement of the granitic rock, and their outer parts, an age of 219±3 Ma for a similar or even the same fluid event. It is thus suggested that the HP‐UHP metamorphism of the Bixiling eclogite facies rocks took place during the Neoproterozoic Jinningian, and the Indosinian age values may only represent a late event in the nature of fluid activity.