摘要
通过矿区构造及一号窿矿体构造研究，论述了湖南石门县界牌峪地区砷矿床一号窿矿体构造特征、矿体特征、矿体与断裂构造的成因联系，指出了矿区的导矿构造与容矿构造，提出了本区中生代３期主要构造应力场。
By studying on the structures of the mine and No. 1 tunnel orebody,this paper discusses the structural feature of No.1 tunnel orebody of the arsenic deposit in Jiepaiyu region in Shimen county of Hunan, the orebody's feature and the genetic connection of the orebody with the fracture structures, it points out the ore directing and ore bearing structures and 3 ages' major tectonic stress field of Mesozoic Era in this region, and it emphasizes that the combination of the partial stress field of the mine with superior joints of relevant direction is the major genetic model of the arsenic deposit in this region.
出处
《广西地质》
1996年第3期7-15,共9页
Guangxi Geology
关键词
控矿因素
找矿方向
砷矿床
矿体构造
tectonic stress field, ore controlling factor,prospecting direction, Shimen arsenic deposit.
