Continental crustal growth processes recorded in the Gangdese Batholith, southern Tibet
The continental crust in the overriding plate of the India-Asia collision zone in southern Tibet
is characterized by an overthickened layer of felsic composition with an underlying granulite …
is characterized by an overthickened layer of felsic composition with an underlying granulite …
[HTML][HTML] Deep entrapment of buoyant magmas by orogenic tectonic stress: Its role in producing continental crust, adakites, and porphyry copper deposits
RR Loucks - Earth-Science Reviews, 2021 - Elsevier
Arc-basaltic melts of typical hydration state (≥ 2 wt% H 2 O) are buoyant relative to all
common crustal igneous rock types and may pass adiabatically from a mantle source …
common crustal igneous rock types and may pass adiabatically from a mantle source …
Growth of continental crust in intra-oceanic and continental-margin arc systems: Analogs for Archean systems
Earth's continental crust has grown and been recycled throughout geologic history along
convergent plate margins. The main locus of continental crustal growth is in intra-oceanic …
convergent plate margins. The main locus of continental crustal growth is in intra-oceanic …
The causes of continental arc flare ups and drivers of episodic magmatic activity in Cordilleran orogenic systems
Continental arcs in Cordilleran orogenic systems display episodic changes in magma
production rate, alternating between flare ups (70–90 km 3 km− 1 Myr− 1) and lulls (< 20 km …
production rate, alternating between flare ups (70–90 km 3 km− 1 Myr− 1) and lulls (< 20 km …
Chemical mohometry: Assessing crustal thickness of ancient orogens using geochemical and isotopic data
P Luffi, MN Ducea - Reviews of Geophysics, 2022 - Wiley Online Library
Convergent plate boundaries are key sites for continental crustal formation and recycling.
Quantifying the evolution of crustal thickness and paleoelevation along ancient convergent …
Quantifying the evolution of crustal thickness and paleoelevation along ancient convergent …
Cenozoic porphyry and other hydrothermal ore deposits along the South Caucasus-West Iranian tectono-magmatic belt: a critical reappraisal of the controlling factors
In this contribution, we investigate the space and time distribution of the Cenozoic
magmatism and the associated porphyry Cu-Mo±Au and other hydrothermal (mostly …
magmatism and the associated porphyry Cu-Mo±Au and other hydrothermal (mostly …
The temporal distribution of Earth's supermountains and their potential link to the rise of atmospheric oxygen and biological evolution
We use the distribution of low-Lu and low-Lu/Dy zircons, derived from the eroded roots of
mountains, where trace amounts of zircon compete with abundant garnets for heavy rare …
mountains, where trace amounts of zircon compete with abundant garnets for heavy rare …
Temporal changes in subduction-to collision-related magmatism in the Neotethyan orogen: The Southeast Iran example
Continental-arc igneous rock compositions change in response to the transition from
subduction to collision and these changes can reveal how the crust, lithosphere and magma …
subduction to collision and these changes can reveal how the crust, lithosphere and magma …
Arclogites and their role in continental evolution; part 2: relationship to batholiths and volcanoes, density and foundering, remelting and long-term storage in the …
Arclogites are eclogite-like rocks formed magmatically as ultramafic residues and cumulates
in the roots of thick arcs (Ducea et al., 2021 companion paper). They are inferred to be …
in the roots of thick arcs (Ducea et al., 2021 companion paper). They are inferred to be …
Wet calc-alkaline magmatic fractionation in the middle–upper crustal sections of the continental arc: Insights from the Neoproterozoic Nanba intrusive complex …
Elucidating the petrological and geochemical characteristics of continental arc crustal
fragments can provide unique insights into the magmatic evolutional path and …
fragments can provide unique insights into the magmatic evolutional path and …