Petrogenesis of mafic‐intermediate dykes from the Central Qilian belt, NW China: Significance of the role of subducted compositions in sub‐arc mantle

• Published in: Geological journal (Chichester, England) Vol. 58; no. 7; pp. 2790 - 2804
• Main Authors: Ma, De‐qing, Wang, Chao, Li, Hang, Zhu, Xiao‐hui, Hao, Jiang‐bo, Yu, Zun‐pu, Sun, Xiao‐kui, Zhang, Shuai, Li, Xue
• Format: Journal Article
• Language: English
• Published: Hoboken, USA John Wiley & Sons, Inc 01.07.2023; Wiley Subscription Services, Inc
• Subjects: Affinity; Belts; Crystallization; Earth mantle; Enrichment; Evolution; Gabbro; Geochemistry; Geochronology; Geochronometry; Heterogeneity; Isotopes; Lava; Mafic‐intermediate dykes; Magma; Niobium; Orogeny; Paleoceanography; Petrogenesis; Qilian orogenic belt; Radiometric dating; Rare earth elements; Ratios; rear‐arc; Rock; Rocks; Rubidium; Sediments; Strontium; Strontium 87; Strontium isotopes; Subduction; subduction components; Thorium; Zircon
• ISSN: 0072-1050; 1099-1034
• DOI: 10.1002/gj.4741

Subduction system in the Qilian orogenic belt experienced the variability of an active continental arc in space and time related to the subduction of the Proto‐Tethys Ocean. Zircon U–Pb geochronology and whole‐rock chemical and Sr–Nd isotopic data of mafic to intermediate dykes in the western part of the Central Qilian belt (WCQB) are used to track magma provenance from compositionally variable reservoirs in the sub‐arc mantle and constrain the magmatic evolution of the rear‐arc at 450–445 Ma. Petrological, whole‐rock chemical and zircon U–Pb dating results reveal that the studied dykes mainly comprise calc‐alkaline lamprophyre (CAL), high Mg# andesitic porphyrite (HMA) and high FeO hornblende gabbro (HFG) with crystallization ages of 447, 453 and 448 Ma, respectively. Among them, CAL and HMA have affinities in high‐K calc‐alkaline suites, high REE contents (∑REE = 131.1–202.3 ppm) with high LaN/YbN values (6.77–17.99), enriched in large‐ion lithophile elements (LILE, e.g., Rb and U), and depleted in high‐field‐strength elements (HFSE, e.g., Nb, Ta, and Ti). They also have high Th/La (0.20–0.46), Th/Nb (0.67–1.64) and Th/Yb (3.88–14.11) ratios, and relatively high whole‐rock initial 87Sr/86Sr ratios (0.707469–0.708493) and εNd(t) values (−4.7 to −3.1). Whereas, HFG is affinities in medium to high‐K calc‐alkaline suites, and has moderate rare earth elements (∑REE = 70.1–112.5 ppm) with flat REE patterns (LaN/YbN = 2.12–3.05) and exhibits enriched LILE, and Sr–Nd isotopes ((87Sr/86Sr)i = 0.713496–0.729216, εNd(t) = −2.93 to +2.04). Such typical “continental” geochemical features of the different K‐rich dykes do not result from crustal assimilation but reflect an enriched mantle source resulting from their mantle heterogeneity due to recycling of different subducted sediments. The temporal evolution of the geochemical characteristics of mafic‐intermediate dykes is consistent with an extension setting triggered by removing the thickened arc crust root in the WCQB. Schematic cartoon showing the rear‐arc extensional event of the southward subduction of the North Qilian Ocean at ca. 450–445 Ma. ca. 450–445 Ma dykes were formed in the rear‐arc region of Central Qilian belt. Dykes reflect an enriched mantle source involving subduction components with sediments.