Ophiolite genesis and global tectonics: Geochemical and tectonic fingerprinting of ancient oceanic lithosphere
Y Dilek, H Furnes - Bulletin, 2011 - pubs.geoscienceworld.org
Ophiolites, and discussions on their origin and significance in Earth's history, have been
instrumental in the formulation, testing, and establishment of hypotheses and theories in …
instrumental in the formulation, testing, and establishment of hypotheses and theories in …
Ridge subduction, magmatism, and metallogenesis
Modern oceans contain large bathymetric highs (spreading oceanic ridges, aseismic ridges
or oceanic plateaus and inactive arc ridges) that, in total, constitute more than 20–30% of the …
or oceanic plateaus and inactive arc ridges) that, in total, constitute more than 20–30% of the …
Ridge subduction and crustal growth in the Central Asian Orogenic Belt: evidence from Late Carboniferous adakites and high-Mg diorites in the western Junggar …
The Central Asian Orogenic Belt (CAOB) is a natural laboratory for the study of accretionary
tectonics and crustal growth owing to its massive generation of juvenile crust in the …
tectonics and crustal growth owing to its massive generation of juvenile crust in the …
Geochemical and geochronological study of early Carboniferous volcanic rocks from the West Junggar: petrogenesis and tectonic implications
H Geng, M Sun, C Yuan, G Zhao, W **ao - Journal of Asian Earth Sciences, 2011 - Elsevier
A series of early Carboniferous volcanic rocks, ie, basalt, andesite, and dacite, occur in the
West Junggar. Zircon U–Pb isotopic data indicate that these rocks coevally erupted at 331 …
West Junggar. Zircon U–Pb isotopic data indicate that these rocks coevally erupted at 331 …
Permian alkaline granites in the Erenhot–Hegenshan belt, northern Inner Mongolia, China: Model of generation, time of emplacement and regional tectonic …
Abstract The Central Asian Orogenic Belt (CAOB) is known to be the Earth's largest
Phanerozoic accretionary orogenic belt. Its southern margin, particularly in the southern …
Phanerozoic accretionary orogenic belt. Its southern margin, particularly in the southern …
Geochronological and geochemical study of the Darbut Ophiolitic Complex in the West Junggar (NW China): implications for petrogenesis and tectonic evolution
G Yang, Y Li, P Gu, B Yang, L Tong, H Zhang - Gondwana Research, 2012 - Elsevier
The Darbut Ophiolitic Complex consists of ultramafic rocks, cumulates, pillow lavas and
abyssal radiolarian cherts, and occurs in the Sartuohai–Suluqiaoke area which is situated in …
abyssal radiolarian cherts, and occurs in the Sartuohai–Suluqiaoke area which is situated in …
Late Silurian–early Devonian adakitic granodiorite, A-type and I-type granites in NW Junggar, NW China: partial melting of mafic lower crust and implications for slab …
Abstract Late Silurian–early Devonian magmatism of the NW Junggar region in the Central
Asian Orogenic Belt provides a critical geological record that is important for unraveling …
Asian Orogenic Belt provides a critical geological record that is important for unraveling …
Geochemistry, zircon U-Pb and Hf isotope for granitoids, NW Sanandaj-Sirjan zone, Iran: Implications for Mesozoic-Cenozoic episodic magmatism during Neo …
Abstract The Sanandaj-Sirjan zone (SSZ) of Iran comprises sedimentary and metamorphic
basement rocks, which are generally regarded as having been derived from the southern …
basement rocks, which are generally regarded as having been derived from the southern …
Petrogenesis of Late Paleoproterozoic Liangcheng charnockites and S-type granites in the central-northern margin of the North China Craton: implications for ridge …
The 1930–1890Ma, garnet-bearing, peraluminous, Liangcheng granitoids are mainly
distributed in the Fengzhen belt in the North China Craton (NCC). They consist of early …
distributed in the Fengzhen belt in the North China Craton (NCC). They consist of early …
Ridge subduction: Unraveling the consequences linked to a slab window development beneath South America at the Chile Triple Junction
The subduction of an active spreading center generates a clear signature in the temporal
evolution of subduction zones. It disrupts the typical arc‐type magmatism and intraplate …
evolution of subduction zones. It disrupts the typical arc‐type magmatism and intraplate …