大兴安岭北部兴隆地区寒武纪侵入岩锆石U-Pb年代学、地球化学及其构造意义

吴宜翰; 刘博; 韩宝福; 巩恩普; 陈家富

doi:10.3799/dqkx.2019.209

Volume 44 Issue 10

Nov. 2019

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Article Navigation > Earth Science > 2019 > 44(10): 3346-3360

Wu Yihan, Liu Bo, Han Baofu, Gong Enpu, Chen Jiafu, 2019. Zircon U-Pb Geochronology and Geochemistry of Cambrian Plutons in Xinglong Area of Northern Da-Hinggan Mountains: Implications for Tectonic Evolution. Earth Science, 44(10): 3346-3360. doi: 10.3799/dqkx.2019.209

Citation:

Wu Yihan, Liu Bo, Han Baofu, Gong Enpu, Chen Jiafu, 2019. Zircon U-Pb Geochronology and Geochemistry of Cambrian Plutons in Xinglong Area of Northern Da-Hinggan Mountains: Implications for Tectonic Evolution. Earth Science, 44(10): 3346-3360. doi: 10.3799/dqkx.2019.209

Citation:

Wu Yihan, Liu Bo, Han Baofu, Gong Enpu, Chen Jiafu, 2019. Zircon U-Pb Geochronology and Geochemistry of Cambrian Plutons in Xinglong Area of Northern Da-Hinggan Mountains: Implications for Tectonic Evolution. Earth Science, 44(10): 3346-3360. doi: 10.3799/dqkx.2019.209

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Zircon U-Pb Geochronology and Geochemistry of Cambrian Plutons in Xinglong Area of Northern Da-Hinggan Mountains: Implications for Tectonic Evolution

doi: 10.3799/dqkx.2019.209

Wu Yihan^1
,,
Liu Bo^{1
,
,},
Han Baofu²,
Gong Enpu¹,
Chen Jiafu¹

1.
Key Laboratory of Ministry of Education on Safe Mining of Deep Metal Mines, College of Resources and Civil Engineering, Northeastern University, Shenyang 110819, China
2.
Key Laboratory of Orogenic Belts and Crustal Evolution of Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing 100871, China

Received Date: 2019-08-18
Publish Date: 2019-11-11

Abstract

Abstract

The Xinglong area in the northern Da-Hinggan Mountains is located in the north of the Xinlin-Xiguitu suture zone and the southern margin of the Erguna block and belongs to the northern Xingmeng orogenic belt. However, the tectonic settings for the Cambrian plutons have been still in debate due to the absence of available data, which hampers our understanding of the early tectonic evolution of Xinlin-Xiguitu Ocean. In this study, it carries out a detailed investigation on the Neihe pluton from the Xinglong area using zircon U-Pb dating and whole-rock geochemistry to constrain the age and petrogenesis, and provides new evidence for solving the problems. The LA-ICP-MS zircon U-Pb ages for the quartz monzonite and pyroxene diorite are 508±3 Ma and 507±5 Ma, respectively, indicating that they were formed during the Middle Cambrian. Geochemically, the quartz monzonite and pyroxene diorite are high-K calc-alkaline and calc-alkaline series, and both are enriched in light rare earth elements and show variable degrees of negative anomalies of Nb, Ta and Ti. The Nb/Ta ratios for the quartz monzonite and pyroxene diorite are 22.41 and 17.12, respectively, and they are low in the contents of the MgO(< 8%) and Mg^# values (42-70). These geochemical features are typical of subduction-related rocks, suggesting that the studied rocks may be generated by partial melting of a primitive mantle source modified by subduction-related fluids. Combined with available data from coeval plutons, ophiolitic mélanges, and blueschists, the Neihe pluton should be generated in an active continental margin setting related to the Cambrian northward subduction of the northern Xinlin-Xiguitu Ocean. New findings provide important evidence for the early subductionrelated tectonic evolution of the Xingmeng orogenic belt.
- Cambrian,
- Erguna block,
- zircon U-Pb geochronology,
- Xinlin-Xiguitu Ocean,
- Xingmeng orogenic belt,
- geochemistry

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References(48)

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