Petrogenesis and tectonic settings of volcanic rocks of the Ashele Cu–Zn deposit in southern Altay, Xinjiang, Northwest China: Insights from zircon U–Pb geochronology, geochemistry and Sr–Nd isotopes. (15th November 2015)

• Record Type: Journal Article
• Authors: Wu, Yufeng; Yang, Fuquan; Liu, Feng; Geng, Xinxia; Li, Qiang; Zheng, Jiahao
• Is Part Of: Journal of Asian earth sciences. Volume 112(2015)
• Page Start: 60
• Page End: 73
• Publication Date: 2015-11-15
• Subjects: Volcanic rocks -- Zircon U–Pb dating -- Geochemistry -- Ashele Formation -- Ridge subduction; Earth sciences -- Asia -- Periodicals; Sciences de la terre -- Asie -- Périodiques; Earth sciences; Asia; Periodicals; 555.05
• DOI: 10.1016/j.jseaes.2015.08.023
• Languages: English
• ISSNs: 1367-9120

Abstract

Highlights: The dacite of the Ashele Formation formed approximately 403 Ma ago. The formation age of the Ashele Formation volcanic rocks is 403–375 Ma. The dacite with high Mg# values showing a sanukitoids affinity. The basalt mainly derived from an N-MORB-type depleted asthenospheric mantle in an island arc setting. The dacites and basalts of Ashele Formation were associated with ridge subduction. Abstract: The Early–Mid-Devonian Ashele Formation of the southern margin of the Chinese Altay hosts the Ashele Cu–Zn volcanogenic massive sulfide (VMS) deposit and consists of intercalated volcanic and sedimentary rocks that have experienced regional greenschist-facies metamorphism. We studied the petrography, zircon U–Pb geochronology, geochemistry, and Sr–Nd isotopes of dacites and basalts in order to understand the petrogenesis of these rocks and the regional tectonic evolution. Two dacites yielded LA-MC-ICP-MS zircon U–Pb ages of 402 ± 6 Ma and 403 ± 2 Ma. The dacites are calc-alkaline, and characterized by high Na2 O/K2 O ratios (3.6–9.3), and high Mg# values (47–63), enrichment in large ion lithophile elements (LILE) and light rare earth elements (LREE), depletion in Nb, Ta, Ti, and P, and relatively positive ε Nd ( t ) values (+3.6 to +7.5), collectively suggesting a sanukitic magma affinity. The variations in the major and trace elements of the dacites indicate that Fe–Ti oxide, plagioclase, and apatite were fractionated during their petrogenesis. The basalts are tholeiitic, and are characterized by high Mg# values (66–73), and negative Nb and Ta anomalies. The geochemical characteristics of the basalts are similar to those of N-MORB. Those characteristics together with the positive ε Nd ( t ) values (+6.8 to +9.2) of the basalts, indicate that the precursor magma was derived mainly from an N-MORB-type depleted asthenospheric mantle in an island arc setting. The geochemical similarities between the basalts and dacites indicate that they both originated from a similar depleted mantle source via partial melting under different magmatic conditions in each case, possibly related to ridge subduction.