Zobrazeno 1 - 10
of 36
pro vyhledávání: '"Yun Deuk Jang"'
Publikováno v:
American Mineralogist. 107:1149-1163
The origin of celadonite still remains enigmatic and fragmentary. Exceptional celadonite mineralization was discovered in the Miocene lacustrine Janggi Basin in the southeastern Korean Peninsula. This Janggi celadonite is a greenish, earthy/vitreous
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c96f0827560e41f27cbb6cc08db72c70
https://doi.org/10.2138/am-2022-8045
https://doi.org/10.2138/am-2022-8045
Publikováno v:
Journal of the Geological Society of Korea. 57:679-690
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::96becb479eb3bf02e6533ab124a57321
https://doi.org/10.14770/jgsk.2021.57.5.679
https://doi.org/10.14770/jgsk.2021.57.5.679
Publikováno v:
Contributions to Mineralogy and Petrology. 177
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::61b89abe2efd14c225916fb5bcd713c3
https://doi.org/10.1007/s00410-022-01951-4
https://doi.org/10.1007/s00410-022-01951-4
Publikováno v:
Lithos. :109-124
The Satkatbong diorite (190 Ma) and the older Yeongdeok granite (250 Ma) in the Yeongnam massif, which is part of the southeastern margin of the Eurasian plate, are affected by a subduction system that is associated with the Izanagi and Farallon plat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aec6d53c7fd68fa75ee4249f4116515c
https://doi.org/10.1016/j.lithos.2018.01.015
https://doi.org/10.1016/j.lithos.2018.01.015
Publikováno v:
Geosciences Journal. 21:1-19
Microstructures developed in the fault gouge zone, Yangbuk, Gyeongju city, Korea, were characterized with emphasis on distribution of remaining grains. Based on XRD analysis, the fault gouges consist of quartz, feldspar and clay minerals composed of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::78a18ef4d52e8ef463e8afbefcc35eeb
https://doi.org/10.1007/s12303-016-0021-1
https://doi.org/10.1007/s12303-016-0021-1
Publikováno v:
Journal of the mineralogical society of korea. 29:123-129
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6b06abc170f9c18aa4c8b85f26425caf
https://doi.org/10.9727/jmsk.2016.29.3.123
https://doi.org/10.9727/jmsk.2016.29.3.123
Publikováno v:
Lithos. :105342
Ulleung Island is an alkaline volcano that consists of Pleistocene basalts (Stage I), effusive trachytes (Stages II–III), and Holocene explosive phonolitic volcanics (Stage IV). Syenites are found as volcanic ejecta in Stage III and IV, hence, acti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ef3c6cd285bc46d2ba13ff7d381ea5bc
https://doi.org/10.1016/j.lithos.2019.105342
https://doi.org/10.1016/j.lithos.2019.105342
Publikováno v:
Journal of Asian Earth Sciences. 188:104089
We present new whole-rock geochemical data for volcanic rocks dredged from active submarine volcanoes TA15, TA16, and TA19 that mark the southern part of the Tonga Arc near Ata island. The lava samples show a wide range of compositions from basalt to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b973c4eb8b3457dc4ad08c767408ffe8
https://doi.org/10.1016/j.jseaes.2019.104089
https://doi.org/10.1016/j.jseaes.2019.104089
Publikováno v:
Journal of the mineralogical society of korea. 28:51-60
We applied gemological analytical approaches on Aquamarine from the Gilgit-Baltistan of Northern Areas, Pakistan. The standard gemological testing indicates that they are consistent with general characteristics of natural aquamarines. We have identif
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fe9586ce8ea641b55e9135c1384a8872
https://doi.org/10.9727/jmsk.2015.28.1.51
https://doi.org/10.9727/jmsk.2015.28.1.51
Autor:
Hyeon Dong Woo, Yun-Deuk Jang
Publikováno v:
The Journal of the Petrological Society of Korea. 23:31-43
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::44c5f39704c88f6139be9addb35e58b2
https://doi.org/10.7854/jpsk.2014.23.2.31
https://doi.org/10.7854/jpsk.2014.23.2.31