Access the full text.
Sign up today, get DeepDyve free for 14 days.
Loading next page...
/lp/wiley/locating-mechanism-of-quartz-vein-gold-deposits-in-rushan-shandong-HET01HgYnM
References (18)
-
(1992)
The genesis of Rushan gold deposit -
(1996)
Lamprophyres ore-forming fluid and H, 0, Sr isotope studies of the Rushan gold deposit -
(1990)
Structural geology. Wuhan: China University of Geology Press -
(1988)
In: Collected Works of the Regional Metallogenic Conditions of China' s Main Types of Gold Ore -
(1989)
Minerallogeny of Gold Ore and Ore-searching in Jiaodong Peninsula -
(1992)
Analysis of regional tectonics -
(1994)
Jiaodong gold mineralization and Jiaolai basin -
(1993)
Magmatic Activities and Gold Mineralization in Western Junggar -
(1996)
Lamprophyres ore-forming fluid and H, 0, Sr isotope studies of the Rushan gold deposit. Mineral Deposits -
(1994)
Geological setting of Jiaodong gold mineralization concentric region -
D. Kitts (1977)
The structure of geology -
(1996)
The Geology and Geochemistry of Gold Deposits of the Greenstone Belt in Jiaodong District -
(1995)
Gold Ore Geology, Lithogenesis and Metallogenesis Related to the Differentiation of Mantlederived C-H-O Fluids in Jiaodong Peninsula -
(1989)
Formation and genesis of Kunyushan complex migmatite , eastern Jiaodong Peninsula , Shandong Province -
(1996)
Study on tectonic-geochemical dynamics of ore-formation in Jiaodong auriferous area -
(1989)
Formation and genesis of Kunyushan complex migmatite, eastern Jiaodong Peninsula -
(1993)
Gold Ore Geology and Geochemistry in Jiaodong Peninsula -
(1985)
Atlas of Tectonophysics Model Experiments
- Publisher
- Wiley
- Copyright
- 1998 Geological Society of China
- ISSN
- 1000-9515
- eISSN
- 1755-6724
- DOI
- 10.1111/j.1755-6724.1998.tb00734.x
- Publisher site
- See Article on Publisher Site
Abstract
Abstract According to the differences in ore‐controlling structural systems and the characteristics of host rocks, textures and structures of ores and mineral associations of ores, quartz vein‐type gold deposits in the Rushan area can be divided into the Rushan and Tongling styles. Rushan style gold deposits, occurring in the Kunyushan complex, include Rushan, Tangjiagou and Tongxishan gold mines. They are distributed along four NNE‐trending and sinistral, compresso‐shear faults with a right stepping array. A prominent characteristic of the gold mineralization is that the orebodies in neighbouring gold deposits distributed in a single ore‐controlling fault zone take opposite pitches. Study of the locating structures of the quartz vein gold deposits shows that the Rushan‐style gold deposits are characterized by NNE and NE zoning. Therefore, the intersections of the NE direction of the known gold deposit and the neighbouring NNE‐trending fault zones are favourable for looking for gold deposits, and the ends of the curving segments of sinistral and right‐stepping faults are favourable for looking for large gold deposits. Tongling‐style gold deposits occur in the Sanfosan porphyritic monzonitic granite. Emplacement of gold deposits is controlled by arcuate and radiate structures formed during the intrusion of the Sanfoshan porphyritic monzonitic granite; the radiate faults controlled the distribution of orebodies and the arcuate faults controlled the pitch of the orebodies.
Journal
Acta Geologica Sinica (English Edition) – Wiley
Published: Mar 1, 1998