Zobrazeno 1 - 10
of 72
pro vyhledávání: '"G. C. Amstutz"'
Publikováno v:
Chinese Journal of Geochemistry. 12:261-269
From the petrological study of ore-hosting rocks which contain large anorthite crystals and the occurrence and chemical composition of anorthites and related minerals, the authors consider that the large anorthite crystals are of authigenic origin.
Autor:
Pan Jiahua, G. C. Amstutz
Publikováno v:
Chinese Journal of Geochemistry. 12:270-288
Sn-polymetallic ores at Dachang, Guangxi Autonomous Region, China, are hosted in Middle-Upper Devonian reef limestones, siliceous rocks, banded and lenticular limestones, etc. Two types of orebodies can be distinguished according to their relations t
Publikováno v:
Mineralium Deposita, Vol. 25 (1990) pp. S136-S140
The Pataz region in the eastern part of the North Peruvian Department La Libertad hosts a number of important gold mining districts like La Lima, El Tingo, Pataz, Parcoy, and Buldibuyo. Economic gold mineralization occurs in quartz-sulfide veins at t
Publikováno v:
Stratabound Ore Deposits in the Andes ISBN: 9783642882845
The Susana copper deposit is located at an elevation of 860 m above sea level in the coastal Cordillera of northern Chile (Carolina de Michilla district), 110 km north of Antofagasta at 70°10′W and 22°40′S. Initial mining began in 1981 by surfa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d9ba3a7fe62af373aec0c727cbef6d58
https://doi.org/10.1007/978-3-642-88282-1_24
https://doi.org/10.1007/978-3-642-88282-1_24
Publikováno v:
Stratabound Ore Deposits in the Andes ISBN: 9783642882845
Stratabound ore deposits in the Andes
Stratabound ore deposits in the Andes pp. 229-251
Stratabound ore deposits in the Andes
Stratabound ore deposits in the Andes pp. 229-251
The Piren Alto Cu-(Zn) massive sulfide occurrence is a minor, noneconomic but genetically interesting ore type of the Paleozoic Coast Range ophiolite (Schira 1990) in south-central Chile. Manto-type massive Sulfides in the greenstone belt south of 38
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::68eaf112ec6b6e2fff5a192eeb505161
https://doi.org/10.1007/978-3-642-88282-1_17
https://doi.org/10.1007/978-3-642-88282-1_17
Autor:
Robert J. Pankhurst, W. Schira, Francisco Hervé, M. Brook, Guillermo Alfaro, Hubert Miller, J. Frutos, G. C. Amstutz
Publikováno v:
Stratabound Ore Deposits in the Andes ISBN: 9783642882845
The coastal range of Chile between 36° and 41 °S (Fig. 1) is mainly composed of low-grade metamorphic rocks developed in a subduction-accretion environment during Paleozoic times.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8be3dddce1109e80356c877e3273cdb6
https://doi.org/10.1007/978-3-642-88282-1_16
https://doi.org/10.1007/978-3-642-88282-1_16
Autor:
E. Lamla, R. Lust, S. Rösinger, H. Preuß, R. Hiltmann, P. Chandra, K. Dose, H. Autrum, E. Kuhn-Schnyder, G. C. Amstutz
Publikováno v:
Naturwissenschaften. 60:556-560
Publikováno v:
Mineralium Deposita. 16:459-465
Autor:
A. N. Ncube, G. C. Amstutz
Publikováno v:
Economic Geology. 76:2047-2052
Autor:
H. H. Kornhuber, E. Schleitzer-Rust, E. Kuhn-Schnyder, G. C. Amstutz, A. Fiechter, K. Cammann, C. K. J�rgensen, L. Jaenicke, V. Neuhoff, E. Gerhards, A. Wacker, K. Seeger, H. Ziegler, O. Hutzinger, E. Seibold
Publikováno v:
Naturwissenschaften. 65:445-448