Zobrazeno 1 - 10
of 28
pro vyhledávání: '"James A. Stimac"'
Autor:
Kushendratno, Christopher J. Harpel, Sofyan Primulyana, James A. Stimac, Cecilia F. Avendaño Rodríguez de Harpel
A VEI 5 dacite eruption emplaced the Orange Tuff about between 34.3 cal kBP and 17.2 cal kBP. Gunung Salak is the unit’s source and the Orange Tuff represents the most recent such eruption from any of the volcanoes southwest of Bogor, Indonesia. Th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::11baf5b3e6d1e62ebfa0f6ab70a1dfa6
https://hdl.handle.net/10356/82733
https://hdl.handle.net/10356/82733
Publikováno v:
Geothermics. 37:332-346
The Awibengkok geothermal field, also known as Salak, is the largest developed geothermal resource in Indonesia, currently sustaining 377 MW of electrical generation. It is a water-dominated, naturally fractured reservoir with benign fluid chemistry.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0e3bc73c199af41e16227194c77685c2
https://doi.org/10.1016/j.geothermics.2008.02.005
https://doi.org/10.1016/j.geothermics.2008.02.005
Autor:
Sergio R. Mejia, Ron Chapman, Adrienne C. L. Larocque, James A. Stimac, Karen Greengrass, Claus Siebe
Publikováno v:
Journal of Volcanology and Geothermal Research. 170:51-60
Volcan Popocatepetl (Popo) is a Quaternary stratovolcano located 70 km SE of Mexico City in the Trans-Mexican Volcanic Belt. The summit crater of Popo is the site of recent ash eruptions, degassing bursts, and dacite-dome growth. Fresh pumice samples
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::645a01eb3466147a13df4666043af145
https://doi.org/10.1016/j.jvolgeores.2007.09.009
https://doi.org/10.1016/j.jvolgeores.2007.09.009
Many geothermal systems are intimately associated with intrusion and volcanism along convergent plate margins, within rifts, and at hot spots. Areas of active structural deformation, especially extension and transtension, localize shallow intrusion a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::35cd7ab5a12c75173ac763467505f7f6
https://doi.org/10.1016/b978-0-12-385938-9.00046-8
https://doi.org/10.1016/b978-0-12-385938-9.00046-8
Autor:
Melissa S. Wilmot, Timothy P. Flood, James A. Stimac, Raymond Patrick R. Maximo, Carmencita B. Arpa, Thomas A. Vogel, Carlo A. Arcilla, Lina C. Patino
Publikováno v:
Contributions to Mineralogy and Petrology. 151:267-281
Silicic volcanic deposits (>65 wt% SiO2), which occur as domes, lavas and pyroclastic deposits, are relatively abundant in the Macolod Corridor, SW Luzon, Philippines. At Makiling stratovolcano, silicic domes occur along the margins of the volcano an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c4bdb725227b2a91523d37e26cf52eec
https://doi.org/10.1007/s00410-005-0050-7
https://doi.org/10.1007/s00410-005-0050-7
Autor:
David R. Hilton, Fraser Goff, Uwe Morgenstern, Dale Counce, James A. Stimac, Adrienne C. L. Larocque
Publikováno v:
Bulletin of Volcanology. 66:149-167
The June 1991 eruption of Mount Pinatubo, Philippines breached a significant, pre-eruptive magmatic-hydrothermal system consisting of a hot (>300 °C) core at two-phase conditions and surrounding, cooler (
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::725ac6919d2952a4534792059f5a3e15
https://doi.org/10.1007/s00445-003-0300-3
https://doi.org/10.1007/s00445-003-0300-3
Publikováno v:
Geothermics. 33:57-86
The Tiwi geothermal field in Southern Luzon, Philippines, has been in commercial operation since 1979, reaching an installed capacity of 330 MW by 1981. The geochemistry of the produced fluids has evolved through a number of reservoir processes that
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8315a2b0c5e0d1475f0ab6b976bda523
https://doi.org/10.1016/j.geothermics.2003.06.004
https://doi.org/10.1016/j.geothermics.2003.06.004
Publikováno v:
Geothermics. 33:87-107
Petrologic analyses of corehole Mat-25 provide a detailed look at the influence of lithology, depth of burial, temperature and hydrothermal fluid chemistry on matrix porosity and permeability in a geothermal system. Average porosity values decline fr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fd2fe7dc3ae8581b1d67894b4ab38ce7
https://doi.org/10.1016/j.geothermics.2003.03.002
https://doi.org/10.1016/j.geothermics.2003.03.002
Autor:
Jennifer A. Jackman, Eric Gauerke, Donald D. Hickmott, James A. Stimac, Adrienne C. L. Larocque, Victor P. Chartrand, G. McMahon
Publikováno v:
Economic Geology. 97:159-164
Magnetite is a common mineral in a wide variety of hydrothermal Au-bearing ore-deposit types. FeTi oxides also occur as phenocrysts in some Au-bearing silicic volcanic rocks. In oxidized plutons, or reduced plutons that are undersaturated with respec
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0a30fe7bcc95c8ee519b99f709d0698b
https://doi.org/10.2113/gsecongeo.97.1.159
https://doi.org/10.2113/gsecongeo.97.1.159
Publikováno v:
The Canadian Mineralogist. 38:1233-1249
Magmatic sulfides are generally accepted as forming by segregation of an immiscible sulfide liquid from a host silicate melt. Immiscible sulfides have been observed in many types of igneous rocks; however, some types of plutonic and volcanic rocks la
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::96195c184c8df3a6be95b26255d35944
https://doi.org/10.2113/gscanmin.38.5.1233
https://doi.org/10.2113/gscanmin.38.5.1233