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Crustal growth and reworking: A case study from the Erguna Massif, eastern Central Asian Orogenic Belt.


ABSTRACT: Despite being the largest accretionary orogen on Earth, the record of crustal growth and reworking of individual microcontinental massifs within the Central Asian Orogenic Belt (CAOB) remain poorly constrained. Here, we focus on zircon records from granitoids in the Erguna Massif to discuss its crustal evolution through time. Proterozoic-Mesozoic granitoids are widespread in the Erguna Massif, and spatiotemporal variations in their zircon ?Hf(t) values and TDM2(Hf) ages reveal the crustal heterogeneity of the massif. Crustal growth curve demonstrates that the initial crust formed in the Mesoarchean, and shows a step-like pattern with three growth periods: 2.9-2.7, 2.1-1.9, and 1.7-0.5 Ga. This suggests that microcontinental massifs in the eastern CAOB have Precambrian basement, contradicting the hypothesis of significant crustal growth during the Phanerozoic. Phases of growth are constrained by multiple tectonic settings related to supercontinent development. Calculated reworked crustal proportions and the reworking curve indicate four reworking periods at 1.86-1.78 Ga, 860-720?Ma, 500-440?Ma, and 300-120?Ma, which limited the growth rate. These periods of reworking account for the crustal heterogeneity of the Erguna Massif.

SUBMITTER: Sun C 

PROVIDER: S-EPMC6881325 | biostudies-literature | 2019 Nov

REPOSITORIES: biostudies-literature

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Crustal growth and reworking: A case study from the Erguna Massif, eastern Central Asian Orogenic Belt.

Sun Chenyang C   Xu Wenliang W   Cawood Peter A PA   Tang Jie J   Zhao Shuo S   Li Yu Y   Zhang Xiaoming X  

Scientific reports 20191127 1


Despite being the largest accretionary orogen on Earth, the record of crustal growth and reworking of individual microcontinental massifs within the Central Asian Orogenic Belt (CAOB) remain poorly constrained. Here, we focus on zircon records from granitoids in the Erguna Massif to discuss its crustal evolution through time. Proterozoic-Mesozoic granitoids are widespread in the Erguna Massif, and spatiotemporal variations in their zircon ε<sub>Hf</sub>(t) values and T<sub>DM2</sub>(Hf) ages rev  ...[more]

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