Zobrazeno 1 - 10
of 26
pro vyhledávání: '"Munjae Park"'
Autor:
Haemyeong Jung, Munjae Park
Publikováno v:
Minerals, Vol 11, Iss 11, p 1152 (2021)
The lattice-preferred orientation (LPO) of minerals is important for interpreting seismic anisotropy [...]
Externí odkaz:
https://doaj.org/article/fcef7c779f7142a1aee05d0a0cb283ed
Publikováno v:
Minerals, Vol 10, Iss 9, p 831 (2020)
Knowledge of the formation and evolution of cratonic subcontinental lithospheric mantle is critical to our understanding of the processes responsible for continental development. Here, we report the deformation microstructures and lattice preferred o
Externí odkaz:
https://doaj.org/article/394f9c5f475d436fa065a507873c9663
Autor:
Munjae Park, Haemyeong Jung
Publikováno v:
Geosciences Journal. 24:679-687
Automated electron backscattered diffraction (EBSD) data yield abundant information on the lattice-preferred orientations (LPOs) and deformation microstructures and mechanisms of minerals in a rock, which aid in our understanding of the tectonic cond
Autor:
Haemyeong Jung, Munjae Park
Publikováno v:
Journal of Geophysical Research: Solid Earth. 124:13168-13191
To understand the relationships between eclogite-facies mineral assemblages, deformation microstructures, and the seismic properties of subducting oceanic crust, eclogites from the Yuka terrane, No...
Publikováno v:
Journal of Geophysical Research: Solid Earth. 126
Autor:
Jinxue Du, Munjae Park, Seungsoon Choi, Dohyun Kim, Haemyeong Jung, Håkon Austrheim, Yong Park, Sejin Jung, Yi Cao
Publikováno v:
Journal of Geophysical Research: Solid Earth. 125
The eclogite in the Flem Gabbro from Flemsøya Island of the Western Gneiss Region in Norway contains atypical eclogitic minerals, such as olivine and orthopyroxene, and can be texturally divided into weakly deformed massive eclogite (MEC) and strong
Publikováno v:
Goldschmidt Abstracts.
Publikováno v:
European Journal of Mineralogy. 29:807-819
Spinel-peridotite xenoliths, hosted in alkali basalts (∼15 Ma), were collected from Adam’s Diggings in the western margin of the Rio Grande Rift (RGR), New Mexico, USA. We selected five representative spinel-peridotite xenoliths, showing abundant
Publikováno v:
Journal of Structural Geology. 145:104309
Crystal preferred orientation (CPO) of high pressure metamorphic rocks is an important contributor to seismic anisotropy in the subduction interface and continental crust. However, the mechanisms of deformation and CPO development, as well as the eff