岩手県松川地熱地帯における岩石の熱水変質

角 清愛

doi:10.11456/shigenchishitsu1951.16.79_261

書誌事項

タイトル別名

Hydrothermal Rock Alteration of Matsukawa Geothermal Area, Iwate Prefecture
その1;地表から深度400mまでの変質

説明

The three-dimensional structure of a hydrothermally altered mass was revealed by deep drillings for the exploitation of the geothermal resources in Matsukawa. The mass comprises five zones of different mineral. assemblages, i. e. weakly altered zone, montmorillonite zone, kaolin zone, alunite zone and pyrophyllite zone, respectively. The three zones, montmorillonite, kaolin and alunite zones, are zonallyarranged. The followings are discussed:<BR>1. The altered mass as a whole is rather vertically elongated reaching to 720m in depth (from the restored surface at the time of main humarolic activity). The shallower part above the 340m level shows a asymmetrical zoning up to the surface. In the deeper part is recognized a symmetrical zoning from conduit to periphery.<BR>2. The amount of discharge of fluid was probaly larger in the deeper part than in the shallower part. The quantities of migrated elements as a whole were generally larger in the shallower part than in the deeper part, although the tendency of migration is similar.

収録刊行物

鉱山地質

鉱山地質 16 (79), 261-271, 1966

資源地質学会

詳細情報詳細情報について

CRID: 1390001206525464064

NII論文ID: 130003441019

DOI: 10.11456/shigenchishitsu1951.16.79_261

ISSN: 00265209

データソース種別

JaLC
CiNii Articles

抄録ライセンスフラグ: 使用不可

書き出し

問題の指摘