Zobrazeno 1 - 8 of 8 pro vyhledávání: '"Loretta D. Dickson"'
1
Tanzurine, Cherry-Red and Emerald-Green Quartz from Tanzania
Autor: Loretta D. Dickson, John S. White
Publikováno v: Rocks & Minerals. 93:250-257
Prepared by William Besse.Following the 2017 Denver mineral and gem shows, one of us (JSW) received a small package in the mail from close friend Elaine Rohrbach. In it were four small quartz piece...
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::a8420f01168566702b3edd663d49a044
https://doi.org/10.1080/00357529.2018.1428863
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5
Quantitative measures of textural anisotropy resulting from magmatic compaction illustrated by a sample from the Palisades sill, New Jersey
Autor: Anthony R. Philpotts, Loretta D. Dickson, Norman H. Gray
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
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6
Millimeter-scale modal layering and the nature of the upper solidification zone in thick flood-basalt flows and other sheets of magma
Autor: Loretta D. Dickson, Anthony R. Philpotts
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
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8
The formation of plagioclase chains during convective transfer in basaltic magma
Autor: Anthony R. Philpotts, Loretta D. Dickson
Publikováno v: Nature. 406(6791)
The basaltic rock in the lower part of the thick Holyoke lava flow in Connecticut and Massachusetts has been shown to have a remarkable texture, with crystals of feldspar linked together in a continuous three-dimensional network of chains1. Heating e
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d62dbaeabd42253c85c7bd9c6536ab85
https://pubmed.ncbi.nlm.nih.gov/10894539
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