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Publication details for Professor Yaoling NiuHe, Z.Y., Xu, X.S. & Niu, Y.L. (2010). Petrogenesis and tectonic significance of a Mesozoic granite–syenite–gabbro association from inland South China. Lithos 119: 621-641.
- Publication type: Journal papers: academic
- ISSN/ISBN: 0024-4937
- DOI: 10.1016/j.lithos.2010.08.016a
- Keywords: Asthenosphere upwelling, Early Yanshanian, Far-field stress, Granite–syenite–gabbro, South China
- View online: Online version
Author(s) from Durham
A granite–syenite–gabbro association from inland South China has been studied for zircon U–Pb ages and Hf
isotopic compositions as well as whole-rock elemental and Sr–Nd isotopic compositions to constrain their
sources and tectonic settings. These rocks have distinctive crystallization ages: the Longyuanba biotite
granites have a mean age of ~240 Ma, the Longyuanba two-mica granites, Pitou alkali-feldspar granites and
amphibole-bearing alkali-feldspar granites, Tabei and Huangbu syenites and Chebu and Chenglong gabbros
have a similar age of ~178 Ma, whereas the Dafengnao syenite gives a mean age of ~165 Ma.
The Longyuanba biotite granites and two-mica granites exhibit S-type characteristics, probably derived from
a Neoproterozoic crustal source. The Chenglong gabbro has OIB-like trace element and highly depleted
isotope compositions (εHf(t)=10.0±1.3; εNd(t)=5.2), suggesting its parental melt to be of asthenospheric
origin with insignificant crustal assimilation. However, crustal contamination is required to explain the
isotopic compositions of the Chebu gabbro. The syenites are shoshonitic in composition, and have depleted
Sr–Nd–Hf isotopic signatures, which we interpret to have resulted from a mixed source of asthenospheric
mantle and metasomatized lithospheric mantle. As expected, the signals of crustal assimilation are
conspicuous in the petrogenesis of the more evolved syenites. The Pitou alkali-feldspar granite and
amphibole-bearing alkali-feldspar granite exhibit I-type and A-type characteristics, respectively. They are
isotopically more depleted than the S-type Longyuanba granites. We suggest that they may have formed
through magma mixing of predominantly mantle-derived melts with the Neoproterozoic crust.
The Jurassic granite–syenite–gabbro association was the product of asthenosphere–lithosphere–crust
interactions, which records the primary role of asthenospheric mantle upwelling in magma generation
both in the mantle and in the crust in the Early Yanshanian time in South China. They probably occurred in
an intraplate rift-like environment as a tectonic response to far-field stress at plate margins during the early
stage of the paleo-Pacific plate subduction. The tectonic transition from the Tethys orogenic regime to the
paleo-Pacific regime was accomplished in the Early Jurassic, and the early Yanshanian magmatism should be
genetically associated with the paleo-Pacific tectonic regime.