Zobrazeno 1 - 10
of 31
pro vyhledávání: '"Paul B. Barton"'
Autor:
Paul B. Barton, Wayne R. Campbell
Publikováno v:
Economic Geology. 100:1313-1324
The rate at which ore deposits form is one of the least well established parameters in all of economic geology. However, increased detail in sampling, improved technology of dating, and sophistication in modeling are reducing the uncertainties and es
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::89f73a673e7453b863616d5a023a81dc
https://doi.org/10.2113/gsecongeo.100.7.1313
https://doi.org/10.2113/gsecongeo.100.7.1313
Autor:
Paul B. Barton, I-Ming Chou
Publikováno v:
Economic Geology. 88:873-884
Pressure is the most important of the intensive parameters for relating epithermal mineralization to the geologic setting. This paper describes the limitations on pressure (and therefore depth) of mineralization that may reasonably be derived from si
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9447afe76b0de00e156e58226180db23
https://doi.org/10.2113/gsecongeo.88.4.873
https://doi.org/10.2113/gsecongeo.88.4.873
Autor:
Chou I-Ming, Paul B. Barton
Publikováno v:
Geochimica et Cosmochimica Acta. 57:2715-2723
The polybaric liquidus surface for the H2O-rich corner of the NaCl-CO2-H2O ternary is calculated, relying heavily on 1. (1) a Henry's law equation for CO2 in brines (modified from Drummond, 1981), 2. (2) the assumption that the contributions of disso
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9a87ff207de500a9a9b2a7f9eacc94d2
https://doi.org/10.1016/0016-7037(93)90385-a
https://doi.org/10.1016/0016-7037(93)90385-a
Publikováno v:
Economic Geology. 87:1911-1918
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aa7bcde6660414ea458d99395a7b5934
https://doi.org/10.2113/gsecongeo.87.7.1911
https://doi.org/10.2113/gsecongeo.87.7.1911
Autor:
Paul B. Barton
Publikováno v:
Mineralogical Magazine. 55:303-315
Over the past several decades, thinking about chemical processes in rocks had been dominated by experimental and theoretical treatments of mineral equilibrium, which is the state from which the time variable has been excluded. But, to an extent excee
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9c8758e406e77974b23b40d13f04668c
https://doi.org/10.1180/minmag.1991.055.380.02
https://doi.org/10.1180/minmag.1991.055.380.02
The filling history, hydrologic budget, and geomorphic development of ancient Lake Creede and its tributary basin are evaluated to determine the factors that controlled its character. The lake filled the Creede caldera that formed in the late Oligoce
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::792b640fdfad546334f82223d13ab959
https://doi.org/10.1130/0-8137-2346-9.105
https://doi.org/10.1130/0-8137-2346-9.105
Autor:
Paul B. Barton, R.A. Ayuso, K.M. Johnson, D.A. Brew, R.J. Goldfarb, B.M. Gamble, E.R. Force, D.A. John, D.A. Lindsey, S.D. Ludington
Publikováno v:
Open-File Report.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::66697b3fb46d98900561a653ea42235e
https://doi.org/10.3133/ofr9582
https://doi.org/10.3133/ofr9582
Publikováno v:
The Journal of Chemical Thermodynamics. 17:481-488
The heat capacity of CuFeS2 (chalcopyrite) was measured between 6.3 and 303.5 K. At 298.15 K, Cp,mo and Smo(T) are (95.67±0.14) J·K−1·mol−1 and (124.9±0.2) J·K−1·mol−1, respectively. From a consideration of the results of two sets of eq
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e52b6f14a832fd8cf56aee1d2a0c3523
https://doi.org/10.1016/0021-9614(85)90147-8
https://doi.org/10.1016/0021-9614(85)90147-8
Autor:
Paul B. Barton
Publikováno v:
Physics and Chemistry of the Earth. :509-528
Ore deposits form under a wide range of physical and chemical conditions, but those precipitating from hot, aqueous fluids—i.e. the hydrothermal deposits—form generally below 700°C and at pressures of only 1 or 2 kbar or less. Natural aqueous fl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ee54239e893ae2444bf79f3dafd86f56
https://doi.org/10.1016/0079-1946(81)90024-0
https://doi.org/10.1016/0079-1946(81)90024-0
Autor:
Paul B. Barton
Publikováno v:
Economic Geology. 66:121-132
The phase relations in the Fe-Sb-S system from 300 degrees to 800 degrees C have been determined using new experimental data on phase assemblages and univariant equilibria in conjunction with information from the literature. Estimates have been made
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3630a7e89d2e601f9e064847f709aa94
https://doi.org/10.2113/gsecongeo.66.1.121
https://doi.org/10.2113/gsecongeo.66.1.121