Carbonatites and alkaline igneous rocks in post-collisional settings: storehouses of rare earth elements
The rare earth elements (REE) are critical raw materials for much of modern technology,
particularly renewable energy infrastructure and electric vehicles that are vital for the energy …
particularly renewable energy infrastructure and electric vehicles that are vital for the energy …
[HTML][HTML] Passive magmatism on Earth and Earth-like planets
Magmatism has occurred throughout Earth's history. From the early Earth to the modern
plate-tectonic Earth, the amount of magmatism has varied, but it has always occurred on …
plate-tectonic Earth, the amount of magmatism has varied, but it has always occurred on …
Continental versus oceanic subduction zones
YF Zheng, YX Chen - National Science Review, 2016 - academic.oup.com
Subduction zones are tectonic expressions of convergent plate margins, where crustal rocks
descend into and interact with the overlying mantle wedge. They are the geodynamic system …
descend into and interact with the overlying mantle wedge. They are the geodynamic system …
Ophiolites in the Xing'an‐Inner Mongolia accretionary belt of the CAOB: Implications for two cycles of seafloor spreading and accretionary orogenic events
Abstract The Xing'an‐Inner Mongolia accretionary belt in the southeastern segment of the
Central Asian Orogenic Belt (CAOB) was produced by the long‐lived subduction and …
Central Asian Orogenic Belt (CAOB) was produced by the long‐lived subduction and …
Melting of subducted continental crust: Geochemical evidence from Mesozoic granitoids in the Dabie-Sulu orogenic belt, east-central China
ZF Zhao, ZB Liu, Q Chen - Journal of Asian Earth Sciences, 2017 - Elsevier
Syn-collisional and postcollisional granitoids are common in collisional orogens, and they
were primarily produced by partial melting of subducted continental crust. This is exemplified …
were primarily produced by partial melting of subducted continental crust. This is exemplified …
Evolution of the Paleo-Tethys Ocean in Eastern Kunlun, North Tibetan Plateau: from continental rift-drift to final closure
The dynamic evolution of the Paleo-Tethys Ocean from continental rift-drift and seafloor
spreading to initial subduction and final closure has been hotly debated. This paper tries to …
spreading to initial subduction and final closure has been hotly debated. This paper tries to …
Petrogenesis of the Wadi El-Faliq Gabbroic Intrusion in the Central Eastern Desert of Egypt: Implications for neoproterozoic post-collisional magmatism associated …
The late Neoproterozoic gabbroic intrusion of the Wadi El-Faliq area in the central Eastern
Desert of Egypt (north Arabian–Nubian Shield; henceforth, ANS) is a fresh, undeformed …
Desert of Egypt (north Arabian–Nubian Shield; henceforth, ANS) is a fresh, undeformed …
Zircon U–Pb geochronology and Sm–Nd and Rb–Sr isotope systematics of Neoproterozoic granitoïds from Bou Azzer (Anti-Atlas-Morocco): the obduction trigger of the …
This study presents new U–Pb zircon ages for the Neoproterozoic granitoids of the Bou
Azzer inlier at the central part of the Anti-Atlas chain (Morocco), in the northwestern edge of …
Azzer inlier at the central part of the Anti-Atlas chain (Morocco), in the northwestern edge of …
Growth of early Paleozoic continental crust linked to the Proto-Tethys subduction and continental collision in the East Kunlun Orogen, northern Tibetan Plateau
L Fu, L Bagas, J Wei, Y Chen, J Chen, X Zhao… - …, 2023 - pubs.geoscienceworld.org
Abstract The East Kunlun Orogen (EKO) in the northern Tibetan Plateau records two
continental collisional orogenic events and magmatism in early Paleozoic and early …
continental collisional orogenic events and magmatism in early Paleozoic and early …