Back-arc magmatism of the Proto-Tethys Ocean in the West Kunlun Orogenic Belt: evidence from the Ordovician Nanpingxueshan Nb-enriched gabbros-Reference-Cited by-同舟云学术

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Back-arc magmatism of the Proto-Tethys Ocean in the West Kunlun Orogenic Belt: evidence from the Ordovician Nanpingxueshan Nb-enriched gabbros

Published:2024-05-19 Issue: Volume: Page:1-21
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Liu Xiao-Qiang¹²,Zhang Chuan-Lin³,Yang Zhi-Hao¹²,Mahemuti Muredili¹²

Affiliation:

1. Xinjiang Key Laboratory for Geodynamic Processes and Metallogenic Prognosis of the Central Asian Orogenic Belt, Urumqi, P.R . China

2. School of Geology and Mining Engineering, Xinjiang University, Urumqi, P.R. China

3. College of Oceanography, Hohai University, Nanjing, P.R. China

Funder

the National Nature Science Foundation of China

the Tianchi Doctoral Programme in the Xinjiang Uygur Autonomous Region

the Open Project of the Xinjiang Uygur Autonomous Key Laboratory

the Key Science Project of the Xinjiang Uygur Autonomous Region

Publisher

Informa UK Limited

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2024.2355624

Reference115 articles.

1. BGMRX. 1993 Regional Geology of Xinjiang Autonomous Region. Beijing: Geological Publishing House p. 155–231. in Chinese.

2. Olivine-poor sources for mantle-derived magmas: Os and Hf isotopic evidence from potassic magmas of the Colorado Plateau

3. Origin of the adakite-high-Nb basalt association and its implications for postsubduction magmatism in Baja California, Mexico

4. Role of recycled oceanic basalt and sediment in generating the Hf–Nd mantle array

5. Hf-Nd input flux in the Izu-Mariana subduction zone and recycling of subducted material in the mantle

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