Multi-stage infiltration of Na-and K-rich fluids from pegmatites at mid-crustal depths as revealed by feldspar replacement textures A Nurdiana, A Okamoto, K Yoshida, M Uno, T Nagaya, N Tsuchiya Lithos 388, 106096, 2021 | 7 | 2021 |
Characteristics of congruent dissolution of silicate minerals enhanced by chelating ligand under ambient conditions J Wang, A Nurdiana, Y Sato, N Watanabe, N Tsuchiya American Mineralogist 109 (6), 1096-1105, 2024 | 1 | 2024 |
Porosity generation via spatially uncoupled dissolution precipitation during plagioclase replacement in quartz undersaturated fluids A Nurdiana, A Okamoto, M Uno, N Tsuchiya Contributions to Mineralogy and Petrology 179 (1), 10, 2024 | 1 | 2024 |
Development of open transport of aqueous fluid from pegmatite revealed by trace elements in garnet A Nurdiana, A Okamoto, M Uno, N Tsuchiya Geofluids 2022 (1), 8786250, 2022 | 1 | 2022 |
Simultaneous replacement of plagioclase by albite and K-feldspar: natural evidence and hydrothermal experiments A Nurdiana, A Okamoto, M Uno, N Tsuchiya EGU General Assembly Conference Abstracts, EGU21-13915, 2021 | | 2021 |
Fluid-rock reactions and porosity generation induced by infiltration of pegmatitic fluids at mid-crustal depths A Nurdiana Tohoku University, 2021 | | 2021 |
Generation of porosity network in plagioclase induced by multistage infiltration of reactive fluids into metamorphic rocks around quartz diorite intrusion at the middle crust A Nurdiana, A Okamoto, M Uno, K Yoshida, T Nagaya, N Tsuchiya AGU Fall Meeting Abstracts 2020, V019-0008, 2020 | | 2020 |