Zobrazeno 1 - 10
of 103
pro vyhledávání: '"A. R. Philpotts"'
Autor:
Anthony R. Philpotts, Jay J. Ague
Building upon the award-winning second edition, this comprehensive textbook provides a fundamental understanding of the formative processes of igneous and metamorphic rocks. Encouraging a deeper comprehension of the subject by explaining the petrolog
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1bc02ce30e26dc5f6c556015a53d4aca
https://doi.org/10.1017/9781108631419
https://doi.org/10.1017/9781108631419
Autor:
Nicholas G. McDonald, Randolph P. Steinen, Steven J. Jaret, Sean T. Kinney, Paul E. Olsen, Anthony R. Philpotts, E. Troy Rasbury
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d2fcfbbfb9d0b599e8b7f9127ad70d4c
https://doi.org/10.1130/abs/2016ne-272509
https://doi.org/10.1130/abs/2016ne-272509
Publikováno v:
Journal of Applied Chemistry. 3:481-486
Chlorination of methyl acrylate in the presence of methanol has been shown to yield a mixture of methyl αβ-dichloropropionate, methyl α-chloro-β-methoxypropionate, methyl β-chloro-α-methoxy-propionate, methyl β-chloropropionate and traces of m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8a1b908e0cd7f6cad1340dd08ec4bfca
https://doi.org/10.1002/jctb.5010031102
https://doi.org/10.1002/jctb.5010031102
Publikováno v:
Journal of Volcanology and Geothermal Research. 161:81-94
A 1.6-m wide Cretaceous camptonite dike on Higby Mountain, Connecticut, contains deformed vesicles that record an initial brief period of steeply upward intrusion followed by a prolonged vertical downward flow of magma prior to solidification. The ca
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::08ccc2f4bb0db3747fe52022718aeeb9
https://doi.org/10.1016/j.jvolgeores.2006.11.006
https://doi.org/10.1016/j.jvolgeores.2006.11.006
Publikováno v:
Journal of Volcanology and Geothermal Research. 145:192-206
The 40-m-thick central part of the Cohassett flow, which was probably emplaced by inflation of an earlier more Ti-rich flow, exhibits textural evidence of crystal-mush compaction during solidification. Although most of the crystallization started in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b2f86ad2af9a12810f2da9542269e622
https://doi.org/10.1016/j.jvolgeores.2005.01.008
https://doi.org/10.1016/j.jvolgeores.2005.01.008
Publikováno v:
Journal of Geoscience Education. 52:172-177
Service-learning practice has been implemented in a number of upper division geoscience courses taught at the University of Connecticut. These courses include engineering geology, environmental geophysics, exploration seismology, and geology and geop
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f722c1fe767602d01069158394166cd9
https://doi.org/10.5408/1089-9995-52.2.172
https://doi.org/10.5408/1089-9995-52.2.172
Publikováno v:
Journal of Petrology. 44:2033-2051
Most phenocryst populations in volcanic rocks, and those preserved in shallow-level igneous intrusions, are clustered (variously referred to as clots, clumps or glomerocrysts). These clusters of crystals are the building blocks that accumulate to for
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e9379882db4f9fba33c8fb165c4ce08a
https://doi.org/10.1093/petrology/egg069
https://doi.org/10.1093/petrology/egg069
Publikováno v:
Journal of Volcanology and Geothermal Research. 121:293-312
Early in the crystallization of many tholeiitic basaltic magmas, plagioclase crystals cluster together into a 3-D cellular network, which forms a passive marker capable of recording the deformation that accompanies compaction of crystal mush. Althoug
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fbda46a767cbea28141223f456500ff7
https://doi.org/10.1016/s0377-0273(02)00463-8
https://doi.org/10.1016/s0377-0273(02)00463-8
Autor:
Alan E. Boudreau, Anthony R. Philpotts
Publikováno v:
Contributions to Mineralogy and Petrology. 144:176-184
Compaction in the Holyoke flood-basalt flow is modeled using a quantitative phase equilibrium routine based on the MELTS algorithm that is coupled with compaction-driven heat and mass transport equations. For a crystal–liquid mush that is cooling f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5a64b79a75ea5a1b2ec4d3a929cfa695
https://doi.org/10.1007/s00410-002-0391-4
https://doi.org/10.1007/s00410-002-0391-4
Publikováno v:
Journal of Structural Geology. 24:1171-1177
Water flooding the surface of the Holyoke flood-basalt flow of Connecticut and Massachusetts was probably responsible for its entablature developing quench textures to depths of 80 m beneath the flow's surface. Despite the rapid cooling from above, t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9549e19ad3434de2c7aee5228cdb31b4
https://doi.org/10.1016/s0191-8141(01)00099-2
https://doi.org/10.1016/s0191-8141(01)00099-2