文献
J-GLOBAL ID:201802238967780653
整理番号:18A0712102
シンマグマせん断帯の最終的運命 冷却花崗岩プルトンにおける破壊と延性流の間の相互作用【JST・京大機械翻訳】
The ultimate fate of a synmagmatic shear zone. Interplay between rupturing and ductile flow in a cooling granite pluton
著者 (6件):
Zibra I.
(Geological Survey of Western Australia, Department of Mines and Petroleum, 100 Plain Street East, Perth, WA, 6004, Australia)
,
Zibra I.
(School of Earth, Atmosphere and Environment, Monash University, Clayton, Victoria, Australia)
,
White J.C.
(Department of Earth Sciences, University of New Brunswick, Fredericton, NB, E3B 5A3, Canada)
,
Menegon L.
(School of Geography, Earth and Environmental Sciences, Plymouth University, Plymouth, PL4 8AA, UK)
,
Dering G.
(Centre for Exploration Targeting (CET), The University of Western Australia, 35 Stirling Highway, Crawley, WA, 6009, Australia)
,
Gessner K.
(Geological Survey of Western Australia, Department of Mines and Petroleum, 100 Plain Street East, Perth, WA, 6004, Australia)
資料名:
Journal of Structural Geology
(Journal of Structural Geology)
巻:
110
ページ:
1-23
発行年:
2018年
JST資料番号:
B0972B
ISSN:
0191-8141
資料種別:
逐次刊行物 (A)
記事区分:
原著論文
発行国:
オランダ (NLD)
言語:
英語 (EN)