Zobrazeno 1 - 10
of 44
pro vyhledávání: '"Bruce B. Hanshaw"'
Publikováno v:
Groundwater as a Geomorphic Agent ISBN: 9781003028833
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::35f32d12498dbecfa00bdfd2bf6548c0
https://doi.org/10.4324/9781003028833-12
https://doi.org/10.4324/9781003028833-12
Publikováno v:
Isotope Techniques in the Hydrologic Cycle
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e6d7c0b9b632dc1e91a5c9450e0d5c4b
https://doi.org/10.1029/gm011p0117
https://doi.org/10.1029/gm011p0117
Publikováno v:
Water Resources Research. 26:1981-2014
Stable isotope data for dissolved carbonate, sulfate, and sulfide are combined with water compo sition data to construct geochemical reaction models along eight flow paths in the Madison aquifer in parts of Wyoming, Montana, and South Dakota. The s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6ed263a02362b2e989d8b27a78a01033
https://doi.org/10.1029/wr026i009p01981
https://doi.org/10.1029/wr026i009p01981
Autor:
Bruce B. Hanshaw, John E. Moore
Publikováno v:
Episodes. 10:315-322
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::62edb29f4c4d2f912aad76d831d21162
https://doi.org/10.18814/epiiugs/1987/v10i4/017
https://doi.org/10.18814/epiiugs/1987/v10i4/017
Autor:
Bruce B. Hanshaw, William Back
Publikováno v:
Journal of Hydrology. 43:287-312
As a result of recent advances by carbonate petrologists and geochemists, hydrologists are provided with new insights into the origin and explanation of many aquifer characteristics and hydrologic phenomena. Some major advances include the recognitio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a0c512f64a31a617f6e900233ab96b1a
https://doi.org/10.1016/0022-1694(79)90177-x
https://doi.org/10.1016/0022-1694(79)90177-x
Autor:
William Back, Bruce B. Hanshaw
Publikováno v:
Hydrological Sciences Journal. 30:257-271
The distribution of permeability and chemical character of groundwater in carbonate aquifers is significantly influenced by the many diagenetic processes and reactions that occur in the early development of these rocks. Many of these diagenetic proce
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c4ca77360124d88325ff031bc6060043
https://doi.org/10.1080/02626668509490988
https://doi.org/10.1080/02626668509490988
Autor:
Robert O. Fournier, Bruce B. Hanshaw
Publikováno v:
Applied Geochemistry. 1:189-197
The chemical and isotopic compositions of hot springs in the San Marcos region of Guatemala are internally consistent with a hydrologic model in which a deep 240°C reservoir and one or more shallow 195–200°C reservoirs are present. Variations in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3db5b4df1ea78ae71adb186d1c99f343
https://doi.org/10.1016/0883-2927(86)90003-x
https://doi.org/10.1016/0883-2927(86)90003-x
Publikováno v:
Geochimica et Cosmochimica Acta. 45:1941-1950
The δ34S values of dissolved sulfide and the sulfur isotope fractionations between dissolved sulfide and sulfate species in Floridan ground water generally correlate with dissolved sulfate concentrations which are related to flow patterns and reside
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7011b7483fd0b9c3523f7ef01e4b2e5a
https://doi.org/10.1016/0016-7037(81)90024-7
https://doi.org/10.1016/0016-7037(81)90024-7
Publikováno v:
Water Resources Research. 15:1521-1535
Xel Ha is a lagoon whose location and morphology are partly controlled by the fracture pattern in upper Pleistocene coral reef limestone. Chemical, isotopic, and hydrologic observations were made nearby where groundwater could be sampled. In addition
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1114534fcfe5e4c4262c03c9ea43e1da
https://doi.org/10.1029/wr015i006p01521
https://doi.org/10.1029/wr015i006p01521
Publikováno v:
Economic Geology. 66:710-724
Most modern disordered dolomite has been found in dynamic environments. However, solutions associated with modern dolomite formation do not have a common Mg/Ca ratio; the ratio ranges from about 3 to 100. Ground-water circulation may have a significa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d3f2a79c7fda2b994c642ca58f3f7e4b
https://doi.org/10.2113/gsecongeo.66.5.710
https://doi.org/10.2113/gsecongeo.66.5.710