Late Silurian to early Devonian development of the Chingiz accretion arc, West Junggar: insights into accretion arc evolution in the Central Asia Orogenic Belt. Issue 17 (22nd November 2021)

• Record Type: Journal Article
• Authors: Chen, Yichao; Zhang, Ji'En; Xiao, Wenjiao; Zhou, Renjie; Song, Shuaihua; Zhang, Zhiyong; Ao, Songjian; Sang, Miao; Zhang, Qian W.L.; Li, Rui; Li, Zhen M.G.; Liu, Yin; Zhang, Hui C.G.; Liu, Jiahui; Wu, Chunming
• Is Part Of: International geology review. Volume 63:Issue 17(2021)
• Page Start: 2083
• Page End: 2103
• Publication Date: 2021-11-22
• Subjects: OPS mélange -- accretion arc -- Chingiz arc -- West Junggar -- CAOB; Geology -- Periodicals; Electronic journals; 551.05
• DOI: 10.1080/00206814.2020.1824128
• Languages: English
• ISSNs: 0020-6814

Abstract

ABSTRACT: Early Palaeozoic evolution of the Kazakhstan orocline in the Central Asian Orogenic Belt (CAOB) is key to reconstructing the Palaeozoic tectonic framework in Central Asia. This study presents field mapping, geochemistry, and geochronological data from the Wulasitai area of northern West Junggar to constrain the subduction polarity and major tectonic events in the Chingiz arc of the Kazakhstan orocline during the Early Palaeozoic. The mapping area outcrops imbricated coherent turbidite slices and mélanges that consist of chert, limestone, silt, sandstone, and conglomerate blocks in mudstone matrix, representing an OPS (Ocean Plate Stratigraphy) mélange in an accretionary complex. Existing fossil ages from these blocks range from the Ordovician to Silurian, while our new detrital zircon U-Pb samples from the turbiditic matrix yield maximum depositional ages (MDTs) from 428 ± 2 Ma to 450 ± 1 Ma. Detrital zircon ages of ~510 to 430 Ma in the mélange suggest the Chingiz arc to the south of the study area as a major sediment source, providing an indirect constraint on the polarity of subduction. We suggest that the northern part of the Chingiz arc may be underlain by southward subduction, with the accretionary complex located on the Wulasitai area of the northern West Junggar. The Wulasitai mélange is overlain depostionally by volcanic rocks carrying depleted HFSE and enriched LILE, LREE. The andesite and tuff are dated to 415 ± 5 Ma, 414 ± 3 Ma, and 402 ± 6 Ma, which we interpret as reflecting the development of the volcanic arc onto the previous subduction complex. This model implies the generation of the arc (accretion arc) as the slab rolling back and trench retreating, which may play an important role in the evolutionary history of CAOB.