Geochemistry of metasedimentary restitic rocks and implications for melting conditions and metal potential of crustal felsic magmas

AS Stepanov, C Allen, SY Jiang, IA Zhukova… - Earth-Science …, 2024 - Elsevier
Partial melting of crustal rocks, also known as anatexis, is the major mechanism of the
fractionation of the continental crust and generation of felsic melts. The segregation of melts …

Multiple timings of garnet-forming high-grade metamorphism in the Neoproterozoic continental collision zone revealed by petrochronology in the Sør Rondane …

F Higashino, T Kawakami, S Sakata, T Hirata - Gondwana Research, 2023 - Elsevier
The Sør Rondane Mountains (SRM), East Antarctica is located in a key area of Gondwana
formation where the East African-Antarctic Orogen and the Kuunga Orogen cross. Timing of …

Ultrahigh–temperature metamorphism and melt inclusions from the Sør Rondane Mountains, East Antarctica

F Higashino, T Kawakami - Journal of Mineralogical and Petrological …, 2022 - jstage.jst.go.jp
This paper reports the first outcrop occurrence of an ultrahigh–temperature (UHT)
metamorphic rock from the Sør Rondane Mountains (SRM), East Antarctica. A pelitic gneiss …

Metamorphic rocks with different pressure-temperature-time paths bounded by a ductile shear zone at Oyayubi ridge, Brattnipene, Sør Rondane Mountains, East …

T Adachi, T Kawakami, F Higashino… - Journal of Mineralogical …, 2023 - jstage.jst.go.jp
The Sør Rondane Mountains, East Antarctica have been thought to be situated in the
collision zone between East and West Gondwana during the final stage of amalgamation of …

Rapid fluid infiltration and permeability enhancement during middle–lower crustal fracturing: Evidence from amphibolite–granulite-facies fluid–rock reaction zones …

D Mindaleva, M Uno, F Higashino, T Nagaya… - Lithos, 2020 - Elsevier
Permeability is a key control on fluid infiltration in the crust. However, quantitative geological
constraints on crustal permeability are limited, particularly with regards to its temporal …

Short‐lived and voluminous fluid‐flow in a single fracture related to seismic events in the middle crust

D Mindaleva, M Uno, N Tsuchiya - Geophysical Research …, 2023 - Wiley Online Library
This study focuses on samples that underwent rapid hydration (∼ 10 hr) and evolved in
permeability (∼ 10− 9 to 10− 8 m2) as a result of crustal fracturing. A coupled reactive …

PetroChron Antarctica: A geological database for interdisciplinary use

G Sanchez, JA Halpin, M Gard… - Geochemistry …, 2021 - Wiley Online Library
Abstract We present PetroChron Antarctica, a new relational database including
petrological, geochemical and geochronological data sets along with computed rock …

Oxygen isotope speedometry in granulite facies garnet recording fluid/melt–rock interaction (Sør Rondane Mountains, East Antarctica)

F Higashino, D Rubatto, T Kawakami… - Journal of …, 2019 - Wiley Online Library
In situ analysis of a garnet porphyroblast from a granulite facies gneiss from Sør Rondane
Mountains, East Antarctica, reveals discontinuous step‐wise zoning in phosphorus and …

Multistage zircon growth recording polyphase metamorphic evolution caused by pulsed granitoid intrusions into a low‐P/T type metamorphic belt: P–T–D–t …

T Kawakami, T Ichino, K Kazuratachi, S Sakata… - Island Arc, 2022 - Wiley Online Library
We report contrasting pressure–temperature–time (P–T–t) paths of migmatites developed in
the highest‐grade metamorphic zone (Grt–Crd zone) and the contact metamorphic zone …

Brine infiltration in the middle to lower crust in a collision zone: mass transfer and microtexture development through wet grain–boundary diffusion

F Higashino, T Kawakami, N Tsuchiya… - Journal of …, 2019 - academic.oup.com
Brine-induced microtexture formation in upper amphibolite to granulite facies lower crust is
investigated using a garnet–hornblende (Grt-Hbl) selvage developed along a planar crack …