Bladed quartz and its relationship to gold mineralization in the Hishikari low-sulfidation epithermal gold deposit, Japan

Jiro Etoh, Eiji Izawa, Koichiro Watanabe, Sachihiro Taguchi, Ryota Sekine

研究成果: ジャーナルへの寄稿記事

26 引用 (Scopus)

抄録

Bladed quartz frequently is observed in low-sulfidation, epithermal gold deposits. Bladed calcite also has been documented in boiling zones of some active epithermal systems, and boiling in these systems has been directly linked to gold mineralization. In the Hishikari low-sulfidation epithermal gold deposit, the distribution and texture of fluid inclusions within bladed quartz reveal a similar relationship to gold precipitation. The formation of bladed quartz at Hishikari involves several stages: (1) deposition of bladed calcite; (2) precipitation of fine-grained adularia and quartz on the surface of calcites blades; (3) dissolution of calcite blades leaving cavities in the interstices between aggregates of adularia and quartz; and (4) infilling of the cavities by later quartz (i.e., pseudomorphs of the original bladed calcite). Bladed quartz is present largely in the deeper part of the vein system, beneath the high-grade gold ore zone at Hishikari. This distribution may be explained by the fact that the original bladed calcite formed at depth in the system, where boiling and loss of CO 2 initially caused the precipitation of the calcite, and quartz formed as pseudomorphs of the original calcite blades.

元の言語英語
ページ(範囲)1841-1851
ページ数11
ジャーナルEconomic Geology
97
発行部数8
DOI
出版物ステータス出版済み - 12 2002

Fingerprint

Gold deposits
sulfidation
Quartz
Calcium Carbonate
calcite
Gold
Japan
quartz
gold
deposits
mineralization
blades
boiling
Boiling liquids
adularia
cavity
interstices
cavities
Carbon Monoxide
veins

All Science Journal Classification (ASJC) codes

  • Geochemistry and Petrology
  • Geophysics

これを引用

Bladed quartz and its relationship to gold mineralization in the Hishikari low-sulfidation epithermal gold deposit, Japan. / Etoh, Jiro; Izawa, Eiji; Watanabe, Koichiro; Taguchi, Sachihiro; Sekine, Ryota.

:: Economic Geology, 巻 97, 番号 8, 12.2002, p. 1841-1851.

研究成果: ジャーナルへの寄稿記事

Etoh, Jiro ; Izawa, Eiji ; Watanabe, Koichiro ; Taguchi, Sachihiro ; Sekine, Ryota. / Bladed quartz and its relationship to gold mineralization in the Hishikari low-sulfidation epithermal gold deposit, Japan. :: Economic Geology. 2002 ; 巻 97, 番号 8. pp. 1841-1851.
@article{2dc11170866b4ebfb5757550961943b0,
title = "Bladed quartz and its relationship to gold mineralization in the Hishikari low-sulfidation epithermal gold deposit, Japan",
abstract = "Bladed quartz frequently is observed in low-sulfidation, epithermal gold deposits. Bladed calcite also has been documented in boiling zones of some active epithermal systems, and boiling in these systems has been directly linked to gold mineralization. In the Hishikari low-sulfidation epithermal gold deposit, the distribution and texture of fluid inclusions within bladed quartz reveal a similar relationship to gold precipitation. The formation of bladed quartz at Hishikari involves several stages: (1) deposition of bladed calcite; (2) precipitation of fine-grained adularia and quartz on the surface of calcites blades; (3) dissolution of calcite blades leaving cavities in the interstices between aggregates of adularia and quartz; and (4) infilling of the cavities by later quartz (i.e., pseudomorphs of the original bladed calcite). Bladed quartz is present largely in the deeper part of the vein system, beneath the high-grade gold ore zone at Hishikari. This distribution may be explained by the fact that the original bladed calcite formed at depth in the system, where boiling and loss of CO 2 initially caused the precipitation of the calcite, and quartz formed as pseudomorphs of the original calcite blades.",
author = "Jiro Etoh and Eiji Izawa and Koichiro Watanabe and Sachihiro Taguchi and Ryota Sekine",
year = "2002",
month = "12",
doi = "10.2113/gsecongeo.97.8.1841",
language = "English",
volume = "97",
pages = "1841--1851",
journal = "Economic Geology",
issn = "0361-0128",
publisher = "Society of Economic Geologists, Inc",
number = "8",

}

TY - JOUR

T1 - Bladed quartz and its relationship to gold mineralization in the Hishikari low-sulfidation epithermal gold deposit, Japan

AU - Etoh, Jiro

AU - Izawa, Eiji

AU - Watanabe, Koichiro

AU - Taguchi, Sachihiro

AU - Sekine, Ryota

PY - 2002/12

Y1 - 2002/12

N2 - Bladed quartz frequently is observed in low-sulfidation, epithermal gold deposits. Bladed calcite also has been documented in boiling zones of some active epithermal systems, and boiling in these systems has been directly linked to gold mineralization. In the Hishikari low-sulfidation epithermal gold deposit, the distribution and texture of fluid inclusions within bladed quartz reveal a similar relationship to gold precipitation. The formation of bladed quartz at Hishikari involves several stages: (1) deposition of bladed calcite; (2) precipitation of fine-grained adularia and quartz on the surface of calcites blades; (3) dissolution of calcite blades leaving cavities in the interstices between aggregates of adularia and quartz; and (4) infilling of the cavities by later quartz (i.e., pseudomorphs of the original bladed calcite). Bladed quartz is present largely in the deeper part of the vein system, beneath the high-grade gold ore zone at Hishikari. This distribution may be explained by the fact that the original bladed calcite formed at depth in the system, where boiling and loss of CO 2 initially caused the precipitation of the calcite, and quartz formed as pseudomorphs of the original calcite blades.

AB - Bladed quartz frequently is observed in low-sulfidation, epithermal gold deposits. Bladed calcite also has been documented in boiling zones of some active epithermal systems, and boiling in these systems has been directly linked to gold mineralization. In the Hishikari low-sulfidation epithermal gold deposit, the distribution and texture of fluid inclusions within bladed quartz reveal a similar relationship to gold precipitation. The formation of bladed quartz at Hishikari involves several stages: (1) deposition of bladed calcite; (2) precipitation of fine-grained adularia and quartz on the surface of calcites blades; (3) dissolution of calcite blades leaving cavities in the interstices between aggregates of adularia and quartz; and (4) infilling of the cavities by later quartz (i.e., pseudomorphs of the original bladed calcite). Bladed quartz is present largely in the deeper part of the vein system, beneath the high-grade gold ore zone at Hishikari. This distribution may be explained by the fact that the original bladed calcite formed at depth in the system, where boiling and loss of CO 2 initially caused the precipitation of the calcite, and quartz formed as pseudomorphs of the original calcite blades.

UR - http://www.scopus.com/inward/record.url?scp=0037991502&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=0037991502&partnerID=8YFLogxK

U2 - 10.2113/gsecongeo.97.8.1841

DO - 10.2113/gsecongeo.97.8.1841

M3 - Article

AN - SCOPUS:0037991502

VL - 97

SP - 1841

EP - 1851

JO - Economic Geology

JF - Economic Geology

SN - 0361-0128

IS - 8

ER -