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- W2363749853 abstract "This paper presents a study of the structural features of a high-temperature W-Sn vein deposit in Nanling Region, Southern China. The deposit occurs in metamorphic rock of a Caledonian folded zone and is believed to have close relation with Eanshanian granites either in age and space as well as in genesis. Ore-contral fracturing, as a result of the new stress conditions in early Eanshanian orogeny, followed the intrusion of granite and was superimposed on some older structures. Two periods may be recognized during the development of ore-bearing fissures, e. g., firstly, the initiation of fissures and, secondly, the opening and mineral filling of them. It has been proved, that the first period took place under a nearly horizontal compressive stress, and the second under a tensile stress when this area was being uplifted. It may be stated that the mineralization as a whole is essentially a process in which the compressive and tensile period alternated repeatedly. The study has also shown that, at this deposit, three stages could be derided in the course of formation of ore-bearing fissures and, on the other hand, four stages in that of ore veins. In general, deformation of each of these stages (periods) bears the carateristies of spacial volume deformation." @default.
- W2363749853 created "2016-06-24" @default.
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- W2363749853 date "1965-01-01" @default.
- W2363749853 modified "2023-09-25" @default.
- W2363749853 title "THE STUDY OF ORE-CONTROLLING STRUCTURES OF A VEIN DEPOSIT" @default.
- W2363749853 hasPublicationYear "1965" @default.
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