Early Miocene metallogenic event formed the Bosawa low‐sulfidation epithermal gold deposit, Northeast Japan arc

IF 1.1 4区 地球科学 Q3 GEOLOGY
Resource Geology Pub Date : 2020-09-21 DOI:10.1111/rge.12248
Teruhiro Suzuki, Shota Satori, Yuho Fujimaki, Yasushi Watanabe
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引用次数: 1

Abstract

There are a number of epithermal Au‐Ag deposits in the Tohoku region of the Northeast Japan arc; however, these deposits have undergone limited exploration for over the past seven decades. This reconnaissance research study of the Bosawa deposit in Akita Prefecture was conducted to support future gold exploration in the Tohoku region. The Bosawa deposit is a vein‐type Au‐Ag deposit, with a production of 42,486 t of ore at 7.01 g/t Au and 14.9 g/t Ag recorded for the period from 1936 to 1957; mining started in the 18th century. The deposit consists of the Ohgiri vein system, which is hosted in felsic volcanic rocks of the Early Miocene Katsurabuchi Formation. The study included geological prospecting, ore description, K‐Ar dating, and fire assay analyses. The deposit is characterized by (a) strongly silicified host lapilli tuff fringed by pyrite‐adularia‐illite alteration; (b) presence of sulfide‐poor banded quartz veins with adularia; (c) abundance of bladed quartz in veins, pseudomorphs after bladed calcite; (d) presence of colloform opal texture in veins; and (e) simple ore mineralogy consisting of gold and argentite. These characteristics are typical of low‐sulfidation epithermal Au deposits. The K‐Ar age of adularia (19.33 ± 0.45 Ma) indicates that mineralization at Bosawa is distinctly older than the ages of other epithermal deposits in the Tohoku region but similar to the age of the initial mineralization episode of the Sado and Tsurushi deposits (24.4–22.1 Ma), Japan's second largest gold producer. This mineralization age coincides with the start of rifting of the Northeast Japan arc and separation from the Asian continent. As the felsic rocks related to this rifting event are widespread in the arc, and some are associated with epithermal gold deposits, the confirmation of typical low‐sulfidation style of mineralization in the Early Miocene provides evidence for a previously unrecognized metallogenic event in the Tohoku region.
早中新世成矿事件形成了日本东北弧渤泽低硫化浅成热液金矿床
在日本东北弧的东北地区有大量的浅成热液型金银矿床;然而,在过去的70年里,这些矿床经历了有限的勘探。对秋田县Bosawa矿床进行了勘查研究,为今后在东北地区进行金矿勘探提供了依据。Bosawa矿床为脉状金银矿床,1936 ~ 1957年记录的产量为42486 t, Au为7.01 g/t, Ag为14.9 g/t;采矿始于18世纪。矿床为大树脉系,赋存于早中新世胜口组长英质火山岩中。该研究包括地质勘探、矿石描述、K - Ar定年和火焰分析。该矿床的特征为:(a)强硅化的寄主石堆凝灰岩,外围是黄铁矿-亚黄铁矿-伊利石蚀变;(b)含硫化物的带状石英脉;(c)叶脉中有丰富的叶状石英,叶状方解石后有假晶;(d)静脉中存在胶状蛋白石织构;(e)由金和辉钼矿组成的简单矿石矿物学。这些特征是低硫化浅成热液型金矿的典型特征。其中,Bosawa的K - Ar年龄(19.33±0.45 Ma)表明,Bosawa的成矿年龄明显高于东北地区其他浅成热液矿床,但与日本第二大金矿Sado和Tsurushi矿床的初始成矿年龄(24.4-22.1 Ma)相似。这一成矿时代与日本东北弧的裂陷开始和与亚洲大陆的分离相吻合。由于与此裂谷事件相关的长英质岩在弧内分布广泛,其中一些与浅成热液型金矿床有关,早中新世典型低硫化型成矿作用的确认为东北地区以前未被认识的成矿事件提供了证据。
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来源期刊
Resource Geology
Resource Geology 地学-地质学
CiteScore
2.30
自引率
14.30%
发文量
18
审稿时长
12 months
期刊介绍: Resource Geology is an international journal focusing on economic geology, geochemistry and environmental geology. Its purpose is to contribute to the promotion of earth sciences related to metallic and non-metallic mineral deposits mainly in Asia, Oceania and the Circum-Pacific region, although other parts of the world are also considered. Launched in 1998 by the Society for Resource Geology, the journal is published quarterly in English, making it more accessible to the international geological community. The journal publishes high quality papers of interest to those engaged in research and exploration of mineral deposits.
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