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Phosphorescence Bay

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Journal Article
Published: 01 January 2002
Reviews in Mineralogy and Geochemistry (2002) 48 (1): 701-742.
.... Fluorescence is here taken to be the same as photoluminescence, i.e., luminescence excited by high energy visible or ultraviolet light, and created by a spin-allowed emission process. Phosphorescence is a term applied to spin-forbidden processes that are generally very slow compared to spin-allowed...
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Journal Article
Published: 24 July 2001
Canadian Journal of Earth Sciences (2001) 38 (7): 1093-1106.
... 000 Eocene or Oligocene sandstone, China Beach, Vancouver Island, British Columbia Muller 1977 CBTS2 1 Tsunami-laid sand, Cultus Bay, Washington, U.S.A. Huntley and Clague 1996 CES-5 12 Glaciomarine sandy clay and silt, Saint-Cesaire, Quebec Lamothe 1996 ; Lamothe and Auclair 1997...
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Journal Article
Published: 10 June 2013
Canadian Journal of Earth Sciences (2013) 50 (9): 930-944.
... a robust, sagittally-oriented bar extending between the corpora calcarea. Rossouw (1984) studied annular growth in Rhinobatos annulatus from Algoa Bay, South Africa, by surface-aging stained centra with silver nitrate. A centrum was collected from the column just ventral to the leading edge...
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Journal Article
Published: 30 October 2012
Geological Magazine (2012) 150 (2): 371-380.
..., 30% calcite and 15% quartz, as established by X-ray diffraction (XRD) analysis at National Museum of Wales). The calcite most likely has strontium inclusions as, during X-ray tomography, the entire rock was phosphorescing slightly. The analysed coral is partially silicified...
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Series: Geological Society, London, Memoirs
Published: 01 January 2011
DOI: 10.1144/M34.9
EISBN: 9781862394094
... in the oceans between the uppermost 500 fathoms (914 m) and the lowest 100 fathoms (184 m). An ingenious deep sea tow net which could be closed at different depths was used and a mass of phosphorescent pelagic organisms, glowing in the dark when the nets were emptied, showed an abundance of life. As previous...
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Journal Article
Published: 01 August 2004
Geochemistry: Exploration, Environment, Analysis (2004) 4 (3): 213-225.
..., and consists of silty clay. The top 2 cm of core CAG-1 is a watery mud with a brown hue, representing the oxic zone. It gradually becomes grey-green with depth and includes the phosphorescent, olive green upper sapropelic layer between 1.70 and 2.10 mbsf interval with relatively high C org contents (up to 1.9...
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Journal Article
Published: 01 January 2014
Reviews in Mineralogy and Geochemistry (2014) 78 (1): 655-690.
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