HUSCAP logo Hokkaido Univ. logo

Hokkaido University Collection of Scholarly and Academic Papers >
Theses >
博士 (理学) >

Study on Wall Rock Alteration Related to Polymetallic Vein-type Deposits,with Special Reference to the Toyoha Mine, Southwest Hokkaido, Japan

Files in This Item:
000000236665.pdf147.49 MBPDFView/Open
Please use this identifier to cite or link to this item:https://doi.org/10.11501/3051980

Title: Study on Wall Rock Alteration Related to Polymetallic Vein-type Deposits,with Special Reference to the Toyoha Mine, Southwest Hokkaido, Japan
Other Titles: 多金属鉱脈鉱床の熱水変質作用 : とくに西南北海道豊羽鉱山について
Authors: Sawai, Osao1 Browse this author
Authors(alt): 澤井, 長雄1
Issue Date: 25-Dec-1990
Publisher: Hokkaido University
Abstract: The Toyoha mine possessing a number of hopeful ore-veins is situated in the suburbs of Sapporo city. The mine has been exploiting polymetallic ores containing abundant lead, zinc, silver and accessory gold,copper,tin,tungsten and indium. Geology of the mining area was re-investigated and new stratigraphy has been accomplished by the present author. Country rocks of the deposits are extensively subjected to various grades of alteration, which were divided into two;diagenetic and hydrothermal origins, then the hydrothermal alteration halo enveloping the ore-veins were precisely studied, i.e. mode of occurrence of the halo, petrochemistry of the altered rocks, mineral chemistry of chlorite and other alteration minerals are reported in this paper. Using sericites KAr ages of the altered rocks were also verified. Results obtained were compared with some typical polymetallic deposits in Japan, and presence of common features in many respects has been confirmed between them. Thus the characterization of the wall rock alteration related to the formation of polymetallic vein-type deposits has been accomplished. Newly obtained informations regarding above-mentioned subjects led to a conclusion that the Toyoha deposits might have been formed by repeated activities of ascending hydrothermal solutions in the periods of Pliocene to Pleistocene.
Conffering University: 北海道大学
Degree Report Number: 乙第3828号
Degree Level: 博士
Degree Discipline: 理学
Type: theses (doctoral)
URI: http://hdl.handle.net/2115/49546
Appears in Collections:学位論文 (Theses) > 博士 (理学)

Submitter: 澤井 長雄

Export metadata:

OAI-PMH ( junii2 , jpcoar_1.0 )

MathJax is now OFF:


 

 - Hokkaido University