Role of arc processes in the formation of continental crust
We review data and recent research on arc composition, focusing on the relatively complete
arc crustal sections in the Jurassic Talkeetna arc (south central Alaska) and the Cretaceous …
arc crustal sections in the Jurassic Talkeetna arc (south central Alaska) and the Cretaceous …
Nature and development of the South Tianshan-Solonker suture zone
HD Li, JB Zhou, SA Wilde - Earth-Science Reviews, 2022 - Elsevier
Abstract The Central Asian Orogenic Belt (CAOB) was generated through multiple collisional
and accretionary events in the Paleo-Asian Ocean, a major global ocean that existed from …
and accretionary events in the Paleo-Asian Ocean, a major global ocean that existed from …
The zircon archive of continent formation through time
NMW Roberts, CJ Spencer - 2015 - pubs.geoscienceworld.org
The strong resilience of the mineral zircon and its ability to host a wealth of isotopic
information make it the best deep-time archive of Earth's continental crust. Zircon is found in …
information make it the best deep-time archive of Earth's continental crust. Zircon is found in …
Ophiolites in the **ng'an‐Inner Mongolia accretionary belt of the CAOB: Implications for two cycles of seafloor spreading and accretionary orogenic events
Abstract The **ng'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 …
[PDF][PDF] Zircon U–Pb and Hf isotopic constraints on the onset time of India-Asia collision
The time of initial collision between India and Asia has been extremely controversial despite
the fact that it is vital to constraining the orogenesis and subsequent evolution of the …
the fact that it is vital to constraining the orogenesis and subsequent evolution of the …
Early‐Middle Triassic high Sr/Y granitoids in the southern Central Asian Orogenic Belt: Implications for ocean closure in accretionary orogens
The key to defining the termination of accretion in an accretionary orogen is to recognize the
initial magmatic processes that are generated at the time of ocean closure. We present new …
initial magmatic processes that are generated at the time of ocean closure. We present new …
Geochronological and Hf isotopic variability of detrital zircons in Paleozoic strata across the accretionary collision zone between the North China craton and …
Abstract The Central Asian orogenic belt formed by accretion subsequent to the contraction
of the paleo–Asian Ocean, and its southeastern segment terminated along the Solonker …
of the paleo–Asian Ocean, and its southeastern segment terminated along the Solonker …
Sedimentary record of the Cretaceous–Paleocene arc–continent collision in the northwestern Colombian Andes: Insights from stratigraphic and provenance …
The collision of intra-oceanic arcs with continental margins is a primary factor controlling the
evolution, modification, and growth of continental crust. Syn-to post-collisional basins are …
evolution, modification, and growth of continental crust. Syn-to post-collisional basins are …
Carboniferous to Triassic polyphase tectonic transition in the western North China craton: A retroarc basin response to termination of the middle segment of the Paleo …
J Sun, Y Dong, J Zhao, Q Chen - Geological Society of …, 2024 - pubs.geoscienceworld.org
Abstract Knowledge of the closure of the archipelago-type southern Paleo-Asian Ocean has
been limited by uncertainty regarding whether the Alxa tectonic belt was isolated from the …
been limited by uncertainty regarding whether the Alxa tectonic belt was isolated from the …
A middle Permian ophiolitic mélange belt in the Solonker suture zone, western Inner Mongolia, China: Implications for the evolution of the Paleo‐Asian Ocean
The Solonker suture zone in the southeastern Central Asian Orogenic Belt is generally
regarded as the location of the final closure of the Paleo‐Asian Ocean, formed by complex …
regarded as the location of the final closure of the Paleo‐Asian Ocean, formed by complex …