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Terrane boundary and spatio-temporal distribution of ore deposits in the Sanjiang Tethyan Orogen: Insights from zircon Hf-isotopic map**
Abstract The Sanjiang Tethyan Orogen (SJTO) of the eastern Tethyan tectonic belt in China
records a transition from Late Paleozoic Tethys realm to Cenozoic continental collision …
records a transition from Late Paleozoic Tethys realm to Cenozoic continental collision …
[HTML][HTML] Geology and genesis of the giant Beiya porphyry–skarn gold deposit, northwestern Yangtze Block, China
J Deng, Q Wang, G Li, Z Hou, C Jiang… - Ore Geology …, 2015 - Elsevier
The Beiya ore deposit is located in the northwestern Yangtze Block, to the southeast of the
Tibetan Plateau, SW China. The deposit is hosted by a porphyritic monzogranitic stock that …
Tibetan Plateau, SW China. The deposit is hosted by a porphyritic monzogranitic stock that …
Tethys tectonic evolution and its bearing on the distribution of important mineral deposits in the Sanjiang region, SW China
The Sanjiang region in SE Tibet Plateau and NW Yunnan is known to have formed by
amalgamation of Gondwana-derived continental blocks and arc terranes as a result of …
amalgamation of Gondwana-derived continental blocks and arc terranes as a result of …
Compositional diversity of ca. 110 Ma magmatism in the northern Lhasa Terrane, Tibet: implications for the magmatic origin and crustal growth in a continent …
The Yanhu area in the northern Lhasa subterrane exposes diverse rock types including
basalts, rhyolites, quartz dioritic porphyries, and associated dioritic enclaves. The basalts …
basalts, rhyolites, quartz dioritic porphyries, and associated dioritic enclaves. The basalts …
Constraining subduction-collision processes of the Paleo-Tethys along the Changning–Menglian Suture: new zircon U-Pb ages and Sr–Nd–Pb–Hf–O isotopes of the …
Abstract The Changning–Menglian suture represents a remnant of the main Paleo-Tethys in
the Sanjiang Orogen (SW China), and preserves abundant magmatic rocks formed during …
the Sanjiang Orogen (SW China), and preserves abundant magmatic rocks formed during …
Slab breakoff triggered ca. 113 Ma magmatism around Xainza area of the Lhasa Terrane, Tibet
Abstract The Lhasa Terrane in southern Tibet is an ideal region to investigate the
geodynamic processes of magmatism in relation to slab breakoff. Here we report zircon …
geodynamic processes of magmatism in relation to slab breakoff. Here we report zircon …
Tin metallogenesis associated with granitoids in the southwestern Sanjiang Tethyan Domain: Nature, deposit types, and tectonic setting
Tin mineralization in the southwestern Sanjiang Tethys Sn metallogenic domain extends
from the Southeast Asia tin belt in the south. The eastern part of the domain does not contain …
from the Southeast Asia tin belt in the south. The eastern part of the domain does not contain …
Origin of the Eocene porphyries and mafic microgranular enclaves from the Beiya porphyry Au polymetallic deposit, western Yunnan, China: Implications for magma …
The origin of magmas with high H 2 O, S and metals that are linked to porphyry economic
mineralization in continental collisional belts is controversial. In this paper, we studied the …
mineralization in continental collisional belts is controversial. In this paper, we studied the …
Geologic and geochemical insights into the formation of the Taiyangshan porphyry copper–molybdenum deposit, Western Qinling Orogenic Belt, China
Taiyangshan is a poorly studied copper–molybdenum deposit located in the Triassic
Western Qinling collisional belt of northwest China. The intrusions exposed in the vicinity of …
Western Qinling collisional belt of northwest China. The intrusions exposed in the vicinity of …
Multiple mineralization events at the Jiru porphyry copper deposit, southern Tibet: Implications for Eocene and Miocene magma sources and resource potential
The Jiru porphyry copper deposit in the Gangdese Porphyry Copper Belt (GPCB) is hosted
by monzogranite and monzogranite porphyry with SHRIMP U–Pb ages of 48.6±0.8 Ma and …
by monzogranite and monzogranite porphyry with SHRIMP U–Pb ages of 48.6±0.8 Ma and …