Zobrazeno 1 - 10
of 125
pro vyhledávání: '"H. Kucha"'
Publikováno v:
Mineral Deposits at the Beginning of the 21st Century ISBN: 9781003077503
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::216a0c9a8a5e74d9977e25fda921f901
https://doi.org/10.1201/9781003077503-37
https://doi.org/10.1201/9781003077503-37
Publikováno v:
Mineral Deposits at the Beginning of the 21st Century ISBN: 9781003077503
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0c4e389e4553ffaf08125665cc366f67
https://doi.org/10.1201/9781003077503-167
https://doi.org/10.1201/9781003077503-167
Autor:
H. Kucha, I.R. Plimer
Publikováno v:
Mineral Deposits at the Beginning of the 21st Century ISBN: 9781003077503
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f8ba9b1397424877f01edca26c0f043f
https://doi.org/10.1201/9781003077503-197
https://doi.org/10.1201/9781003077503-197
Publikováno v:
Mineral Deposits at the Beginning of the 21st Century ISBN: 9781003077503
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5fe769b482229087e002d46c8d82ef8d
https://doi.org/10.1201/9781003077503-38
https://doi.org/10.1201/9781003077503-38
Publikováno v:
Mineral Deposits at the Beginning of the 21st Century ISBN: 9781003077503
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::388f8d992f636b738f351302c58b8857
https://doi.org/10.1201/9781003077503-36
https://doi.org/10.1201/9781003077503-36
Publikováno v:
Acta Geologica Sinica - English Edition. 75:66-73
Previous studies have shown that the ascending, oxidizing brines play a very important role in Kupferschiefer mineralization. Fractures could be the pathway of the brines. In order to clarify the influences of the brines on bulk organic matter, aroma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::79278d8e11efef49503904774c5e2da2
https://doi.org/10.1111/j.1755-6724.2001.tb00508.x
https://doi.org/10.1111/j.1755-6724.2001.tb00508.x
Publikováno v:
Economic Geology. 105:1005-1023
Microglobular sphalerite (90–180 μm) is a major form of sphalerite in the abandoned, Triassic carbonate-hosted Zn-Pb deposit at Bleiberg, Austria. It is common in ores from the Crest horizon and the first Cardita horizon, which contain about 0.5-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6cdd11fbb3ee5b9f19757259e71cf0c7
https://doi.org/10.2113/econgeo.105.5.1005
https://doi.org/10.2113/econgeo.105.5.1005
Autor:
H. Kucha, Johann G. Raith
Publikováno v:
Ore Geology Reviews. 35:87-100
Native gold and unusual gold-oxysulphides, both associated with tetrahedrite, occur in several abandoned copper deposits in the low grade Palaeozoic Greywacke Zone in the Eastern Alps. The ore mineralogy, the mineral chemistry and fluid inclusions in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::49cb205bd8d569b7b53dbf1ee97e5021
https://doi.org/10.1016/j.oregeorev.2008.10.004
https://doi.org/10.1016/j.oregeorev.2008.10.004
Publikováno v:
Mineralium Deposita. 40:123-126
Polished ore samples from the world-class Bleiberg lead-zinc deposit in Austria were studied by Field Emission Scanning Electron Microscopy (FESEM) at magnifications in the range of 105–106. The zinc ore shows nano-sized sphalerite filaments and sp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fe15a973df27778d7075e3b6d1c1b5f5
https://doi.org/10.1007/s00126-005-0473-0
https://doi.org/10.1007/s00126-005-0473-0
Publikováno v:
Economic Geology. 98:1487-1495
Fluid flow models previously proposed have been unable to account for the 350 Mt of copper metal associated with the Kupferschiefer shales in the southwest part of the Polish basin without an unreasonably high concentration of Cu in the brine transpo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2c07a5305e933be095a5aca609243703
https://doi.org/10.2113/gsecongeo.98.7.1487
https://doi.org/10.2113/gsecongeo.98.7.1487