Zobrazeno 1 - 10
of 30
pro vyhledávání: '"A. E. Bence"'
Publikováno v:
Environmental Forensics. 3:331-340
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9eab7d4c6773c5520bce06a5e0374020
https://doi.org/10.1080/713848391
https://doi.org/10.1080/713848391
Total Organic Carbon, an Important Tool in an Holistic Approach to Hydrocarbon Source Fingerprinting
Autor:
P. D. Boehm, W. A. Burns, D. S. Page, A. E. Bence, P. J. Mankiewicz, J. S. Brown, G. S. Douglas
Publikováno v:
Environmental Forensics. 3:243-250
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d3c38842b5494aba99f5f88002d3a852
https://doi.org/10.1080/713848376
https://doi.org/10.1080/713848376
Publikováno v:
1977, Reviews of Lunar Sciences ISBN: 9781118782118
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c47e967ebf2d17bba448e75c2e84d86a
https://doi.org/10.1002/9781118782118.ch14
https://doi.org/10.1002/9781118782118.ch14
Publikováno v:
Anales de la Catedra de Patologia y Clinica de la Tuberculosis. 7
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=pmid________::b855ec331572c75cc5ec47d1d8abbb43
https://pubmed.ncbi.nlm.nih.gov/20984415
https://pubmed.ncbi.nlm.nih.gov/20984415
Publikováno v:
Precambrian Research. 10:249-279
Basalt magmas, derived by the partial melting of planetary interiors, have compositions that reflect the pre-accretionary history of the material from which the planet formed, the planets, subsequent evolutionary history, the chemistry and mineralogy
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dbb902810be182d3724ae9c602ec6d97
https://doi.org/10.1016/0301-9268(80)90014-5
https://doi.org/10.1016/0301-9268(80)90014-5
Publikováno v:
Journal of Geophysical Research. 81:4305-4325
Basalts recovered from sites 100 and 105 of leg 11 of the Deep-Sea Drilling Project are mineralogically and chemically similar to basalts recovered from ridge and near-ridge sites. Textural evidence suggests that the units sampled were extruded as th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::db8a088d9d67be7b6c8d8a6b06a0f586
https://doi.org/10.1029/jb081i023p04305
https://doi.org/10.1029/jb081i023p04305
Autor:
J. J. Papike, A. E. Bence
Publikováno v:
Geophysical Research Letters. 5:803-806
Major differences which exist between terrestrial midocean ridge basalts (MORBs) and lunar mare basalts reflect the different planetary characteristics of earth and moon. MORBs are enriched in aluminum and have higher Mg/(Mg + Fe(2+)). These features
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::393b2dcf8be8ce71c34e4e1ade0a303b
https://doi.org/10.1029/gl005i009p00803
https://doi.org/10.1029/gl005i009p00803
Publikováno v:
Earth and Planetary Science Letters. 58:330-344
Granodiorite and diorite plutons of the Rosetown complex, N.Y., which are associated with the nearby Cortlandt complex, have chemical and textural characteristics indicating that large-scale liquid immiscibility played a major role in their petrogene
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::80b2dfb98173b66ecd9539bab24e22f1
https://doi.org/10.1016/0012-821x(82)90084-x
https://doi.org/10.1016/0012-821x(82)90084-x
Autor:
A. E. Bence, Bruce E. Taylor
Publikováno v:
Economic Geology. 80:2164-2176
West Shasta district bimodal volcanics (Copley Greenstone and Balaklala Rhyolite) are members of a low K calc-alkaline suite. They have rare earth element distributions characterized by pronounced light rare earth element depletion and unfractionated
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::25fca67b326a198be2c5201f6a896995
https://doi.org/10.2113/gsecongeo.80.8.2164
https://doi.org/10.2113/gsecongeo.80.8.2164
Autor:
Martin R. Fisk, A E Bence
Publikováno v:
Earth and Planetary Science Letters. 48:111-123
FAMOUS basalt 527-1-1 (a high-Mg oceanic pillow basalt) has three generations of spinel which can be distinguished petrographically and chemically. The first generation (Group I) have reaction coronas and are high in Al2O3. The second generation (Gro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fa8324ee6b33a6b22cd31be40bcbba93
https://doi.org/10.1016/0012-821x(80)90174-0
https://doi.org/10.1016/0012-821x(80)90174-0