학술논문
Mineralogical and geochemical characteristics of the fault gouge at the Tase outcrop, the Atera Fault / 阿寺断層田瀬露頭における断層ガウジの鉱物学的・地球化学的特徴
Document Type
Journal Article
Author
Source
活断層研究 / Active Fault Research. 2015, 2015(43):1
Subject
Language
Japanese
ISSN
0918-1024
2186-5337
2186-5337
Abstract
We investigated structural, mineralogical and geochemical characteristics of the fault rocks from the active Atera fault, Gifu Prefecture, Japan. We recognized three dominant structural zones at the Tase outcrop: light gray fault gouge, brown fault gouge and black fault breccia. The light gray fault gouge is mainly composed of clay minerals, and exhibited intense shear foliation. The brown fault gouge shows the clearest linear continuity at the outcrop, cutting other structural zones, but the degree of shearing in this zone is relatively weak. The black fault breccia is composed of rock fragments, originated from surrounding host rocks, and black matrix. Fault rocks in these structural zones show fluid-mobile trace element compositions essentially consistent with those of host rocks, indicating that no fluid–rock interaction at high temperatures above 250 ºC took place in these fault zones.