Journal of Jilin University(Earth Science Edition) ›› 2019, Vol. 49 ›› Issue (4): 1015-1038.doi: 10.13278/j.cnki.jjuese.20180014

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Early Paleozoic Tectonic Evolution of Northern Yili Block: Evidence from Diorite in Wenquan, Xinjiang

Jia Yinggang1,2, Zhao Jun2, Jiang Lei2, Guan Liwei2, Wang Xiaoxuan1, He Liang1,2   

  1. 1. School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China;
    2. No.8 Gold Geological Party, CAPF(Center of Urumqi Natural Resources Comprehensive Survey, CGS), Urumqi 830057, China
  • Received:2018-01-18 Online:2019-07-26 Published:2019-07-26
  • Supported by:
    Supported by Geological Survey Projects of China Geological Survey (DD12120115041301)

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Abstract: Located at the junction of Yili block and Siberia plate, the northern Yili block develops a belt of Early Paleozoic intrusive rocks, which are the key to study the northern Yili block tectonic setting and evolution of the old Junggar Ocean. On the basis of a field geological survey and petrographic observation, we present the whole-rock data, U-Pb ages and Hf isotopic data for the Early Paleozoic diorite from Wenquan of northern edge of Yili block. The weighted mean 206Pb/238U ages of the zircons from quartz diorite are(467.7±5.4)Ma,(457.1±3.9) Ma and(455.4±5.0) Ma, indicating that these diorite bodies crystallized from the Early Ordovician to the Middle Ordovician. The petrological and chemical composition show that these diorites are characterized by low SiO2 (50.19%-61.91%, average 56.57%) and TiO2 (0.84%-1.13%, average 1.01%), slightly higher MgO (2.36%-8.17%, average 4.60%), CaO (3.94%-9.45%, average 6.50%), total alkali (Na2O+K2O) (3.74%-7.06%, average 5.41%). The ratio of Na2O/K2O is high (1.42-4.90, average 2.76), while the ratio of A/CNK is low (0.70-0.95, average 0.84). The geochemical data suggest that these diorite bodies belong to quasia-luminous series. The diorites are enriched in large ion lithophile elements (K,Rb), but depleted of high field strength elements (Ta, Nb, Ti). The REE pattern shows a trend of "left high and right low" with minor negative Eu anomalies (0.67-1.12, average 0.90), and heavy REE content is low, indicating the geochemical characteristics of arc igneous rocks in continental margin. Various binary diagrams reveal fractional crystallization of olivine, clinopyroxene, and hornblende. The existence of stratigraphic xenoliths and the La/Sm value (2.99-8.59, average 5.95) suggest the limited crustal contamination during the magma rise. The zircon Hf isotopic compositions of the quartz diorite are mainly characterized by εHf (t) values of 3.9-7.0, two-stage model ages of 991-1 191 Ma (average 1 083 Ma), which is older than U-Pb age. The petrological, geochemical data and zircon Hf isotopic compositions imply that the primary magma derived from a depleted mantle probably mixed with metasomatic enriched lithospheric mantle components and the early fluid metasomatism of oceanic plate. Based on the regional magmatism and the previous study, the authors infer that the old Junggar Ocean crust subducted southward beneath the northern edge of Yili block during 467.7 Ma-455.4 Ma, and ended in the Late Ordovician-Early Silurian.

Key words: zircon U-Pb dating, Hf isotope, diorite, Early Paleozoic, Yili block

CLC Number: 

  • P631.84
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