Results 91 to 100 of about 5,189,165 (162)
The occurrence of ophiolites in the Beishan Orogenic Belt (BOB), located in the southern Central Asian Orogenic Belt (CAOB), is critical for elucidating the tectonic evolution of the southern part of the Paleo-Asian Ocean (PAO).
Lei Wu +17 more
doaj +1 more source
: The Central Asian Orogenic Belt (CAOB) is one of the largest and best preserved accretionary type orogenic belts in the world. Due to its complex tectonic history, the timing and location of the final closure of the Paleo-Asian Ocean and its tectonic ...
Sen Wang +5 more
doaj +1 more source
Two distinct Paleozoic metamorphic events in the Tarim-North China Collage. [PDF]
Soldner J.
europepmc +1 more source
Mapping uncovered a multi-phase arc-back-arc system in the southern Beishan during the Permian. [PDF]
Hong T +4 more
europepmc +1 more source
A number of Permian to Triassic mafic-ultramafic intrusions along the central Asian orogenic belt (CAOB) host either economically important or potential Ni-Cu sulfide mineralization.
Wang, Christina Yan +2 more
core +1 more source
Northeast China, situated in the eastern Central Asian Orogenic Belt (CAOB), marks the terminal closure zone of the Paleo-Asian Ocean (PAO) (eastern segment).
Penghui Zhang +5 more
doaj +1 more source
Survived and disappeared intra-oceanic arcs of the Paleo-Asian Ocean: evidence from Kazakhstan. [PDF]
Safonova I, Perfilova A.
europepmc +1 more source
Late Carboniferous is a critical period in terms of the tectonic evolution of the Central Asian Orogenic Belt (CAOB). In this study, we report the petrology, geochronology and geochemistry of Late Carboniferous mafic to felsic rocks from southern ...
Li, Zhihua +5 more
core +1 more source
Rollback, scissor-like closure of the Mongol-Okhotsk Ocean and formation of an orocline: magmatic migration based on a large archive of age data. [PDF]
Wang T +8 more
europepmc +1 more source
Voluminous continental growth of the Altaids and its control on metallogeny. [PDF]
Wang T +7 more
europepmc +1 more source

