[HTML][HTML] Late Jurassic–Cenozoic reconstructions of the Indonesian region and the Indian Ocean

R Hall - Tectonophysics, 2012 - Elsevier
The heterogeneous Sundaland region was assembled by closure of Tethyan oceans and
addition of continental fragments. Its Mesozoic and Cenozoic history is illustrated by a new …

Nature of parent rocks, mineralization styles and ore genesis of regolith-hosted REE deposits in South China: An integrated genetic model

YHM Li, WW Zhao, MF Zhou - Journal of Asian Earth Sciences, 2017 - Elsevier
Regolith-hosted rare earth element (REE) deposits, also called ion-adsorption or weathered
crust elution-deposited REE deposits are distributed over Jiangxi, Guangdong, Fujian …

Phanerozoic tectonics of the South China Block: Key observations and controversies

Y Wang, W Fan, G Zhang, Y Zhang - Gondwana Research, 2013 - Elsevier
The Phanerozoic tectonic regimes of the South China Block (SCB) hold a key to
understanding of its geodynamic evolution with respect to formation of numerous mineral …

Protolith-related thermal controls on the decoupling of Sn and W in Sn-W metallogenic provinces: Insights from the Nanling region, China

S Yuan, AE Williams-Jones, RL Romer… - Economic …, 2019 - pubs.geoscienceworld.org
Abstract The Nanling region of South China hosts the largest W-Sn metallogenic province in
the world, accounting for more than 54% of global tungsten resources as well as important …

Late Cretaceous–early Palaeogene tectonic development of SE Asia

CK Morley - Earth-Science Reviews, 2012 - Elsevier
The Late Cretaceous–Early Palaeogene history of the continental core of SE Asia
(Sundaland) marks the time prior to collision of India with Asia when SE Asia, from the …

Oxygen fugacity and porphyry mineralization: A zircon perspective of Dexing porphyry Cu deposit, China

C Zhang, W Sun, J Wang, L Zhang, S Sun… - … et Cosmochimica Acta, 2017 - Elsevier
Oxygen fugacity (fO 2) is a key factor that controls the formation of porphyry Cu deposits.
Porphyry Cu deposits are typically oxidized, but when and how porphyry magmas gain their …

Formation of high δ18O fayalite-bearing A-type granite by high-temperature melting of granulitic metasedimentary rocks, southern China

HQ Huang, XH Li, WX Li, ZX Li - Geology, 2011 - pubs.geoscienceworld.org
The genesis of A-type granites has been controversial. Fayalite granite is a member of the
most reduced A-type granites, commonly thought to have been primarily sourced from …

Petrogenesis and tectonic implications of Early Cretaceous S-and A-type granites in the northwest of the Gan-Hang rift, SE China

YH Jiang, P Zhao, Q Zhou, SY Liao, GD ** - Lithos, 2011 - Elsevier
The Gan-Hang rift, trending at least 450km in a NE–SW direction, is a part of a Mesozoic
Basin and Range Province in southeastern China. Detailed SHRIMP zircon U–Pb …

Geochemical and Sr–Nd–Hf isotopic constraints on the origin of Late Triassic granitoids from the Qinling orogen, central China: implications for a continental arc to …

YH Jiang, GD **, SY Liao, Q Zhou, P Zhao - Lithos, 2010 - Elsevier
The Qinling–Dabie–Sulu orogen marks the junction between the North and South China
Blocks. However, the exact timing of the final coalescence of the North and South China …

Mesozoic tectono-magmatic activities in South China: Retrospect and prospect

JR Mao, ZL Li, HM Ye - Science China Earth Sciences, 2014 - Springer
Abstract The South China Block was formed through the collisional orogeny between the
Cathaysia Block and the Yangtze Block in the Early Neoproterozoic. The northern, western …