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Geochronology and geochemistry of igneous rocks from the Kongling terrane: Implications for Mesoarchean to Paleoproterozoic crustal evolution of the Yangtze Block

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TLDR
The Kongling terrane is a high grade metamorphic complex, exposed in the northern part of the Yangtze Block, which mainly consists of TTG gneisses, amphibolites, migmatite, granite and diabase as discussed by the authors.
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This article is published in Precambrian Research.The article was published on 2014-12-01. It has received 119 citations till now. The article focuses on the topics: Migmatite & Terrane.

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Tectonic architecture and multiple orogeny of the Qinling Orogenic Belt, Central China

TL;DR: The Qinling Orogenic Belt (QOB) as mentioned in this paper is a composite orogenic belt that witnessed four major episodes of accretion and collision between discrete continental blocks, such as the North China Block, North Qinling Block and the South China Block.
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Episodic Paleoarchean-Paleoproterozoic (3.3-2.0 Ga) granitoid magmatism in Yangtze Craton, South China: Implications for late Archean tectonics

TL;DR: In this paper, the authors present petrography, geochemistry, zircon U-Pb geochronology and Lu-Hf isotopes of twelve gneissic granitoids from the Archean Kongling Terrane, including trondhjemites, biotite-granites, and two-mica granites.
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Deconstructing South China and consequences for reconstructing Nuna and Rodinia

TL;DR: In this paper, the authors defined four lithotectonic domains: Kongling, Kunming-Hainan, Wuyi, and Coastal domains, which are characterized by isolated Archean to early Paleoproterozoic rock units and events and crop out in northern and southern South China, respectively.
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Zircon U–Pb chronology, Hf isotope analysis and whole-rock geochemistry for the Neoarchean-Paleoproterozoic Yudongzi complex, northwestern margin of the Yangtze craton, China

TL;DR: The Yudongzi complex was probably involved in the amalgamation of the Paleoproterozoic supercontinent Columbia, and affected by a post-collisional metamorphic event at ca. 2.80-3.10-Ga as discussed by the authors.
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Ca. 830 Ma back-arc type volcanic rocks in the eastern part of the Jiangnan orogen: Implications for the Neoproterozoic tectonic evolution of South China Block

TL;DR: In this paper, a combined study of geochronology and geochemistry for the bimodal association of basalts and rhyolitic tuffs from the Shuangqiaoshan Group in south Anhui Province was carried out.
References
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Chemical and isotopic systematics of oceanic basalt : implications for mantle composition and processes

S. S. Sun
TL;DR: In this article, trace-element data for mid-ocean ridge basalts and ocean island basalts are used to formulate chemical systematics for oceanic basalts, interpreted in terms of partial-melting conditions, variations in residual mineralogy, involvement of subducted sediment, recycling of oceanic lithosphere and processes within the low velocity zone.
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Trace element discrimination diagrams for the tectonic interpretation of granitic rocks

TL;DR: In this article, a data bank containing over 600 high quality trace element analyses of granites from known settings was used to demonstrate using ORG-normalized geochemical patterns and element-SiO2 plots that most of these granite groups exhibit distinctive trace element characteristics.
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A Guide to the Chemical Classification of the Common Volcanic Rocks

TL;DR: In this paper, a system was presented whereby volcanic rocks may be classified chemically as follows: Subalkaline Rocks:A.B. Tholeiitic basalt series:Tholeitic picrite-basalt; tholeiite, tholeitic andesite; dacite; rhyolite.
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Geochemical discrimination of different magma series and their differentiation products using immobile elements

TL;DR: In this article, the abundance and distribution of selected minor and trace elements (Ti, Zr, Y, Nb, Ce, Ga and Sc) in fresh volcanic rocks can be used to classify the differentiation products of subalkaline and alkaline magma series in a similar manner to methods using normative or major-element indices.
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