954 resultados para Walker, Robert J. (Robert John), 1801-1869.
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Results are presented of an examination of flow rock-covered Paleoloithic cave art using time-domain terahertz reflectometry.
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Terahertz (THz) radiation is being developed as a tool for the analysis of cultural heritage, and due to recent advances in technology is now available commercially in systems which can be deployed for field analysis. The radiation is capable of penetrating up to one centimetre of wall plaster and is delivered in ultrafast pulses which are reflected from layers within this region. The technique is non-contact, non-invasive and non-destructive. While sub-surface radar is able to penetrate over a metre of wall plaster, producing details of internal structures, infrared and ultraviolet techniques produce information about the surface layers of wall plaster. THz radiation is able to provide information about the interim region of up to approximately one centimetre into the wall surface. Data from Chartres Cathedral, France, Riga Dome Cathedral, Latvia, and Chartreuse du Val de Bénédiction, France is presented each with different research questions. The presence of sub-surface paint layers was expected from documentary evidence, dating to the 13th Century, at Chartres Cathedral. In contrast, at the Riga Dome Cathedral surface painting had been obscured as recently as 1941 during the Russian occupation of Latvia using white lead-based paint. In the 13th Century, wall paintings at the Chapel of the Frescos, Chartreuse du Val de Benediction in Villeneuve les Avignon were constructed using sinopia under-painting on plaster covering uneven stonework.. This paper compares and contrasts the ability of THz radiation to provide information about sub-surface features in churches and Cathedrals across Europe by analysing depth based profiles gained from the reflected signal. © (2013) COPYRIGHT Society of Photo-Optical Instrumentation Engineers (SPIE).
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TOC: Clubs & Organizations…18 / Current Events & Music…30 / Faculty & Staff…33 / Activities & Events… / Honors & Graduation…65 / Graduates…75 / Yearbook Credits…111 / A Thank You…112 YEARBOOK COMMITTEE: Project Director, Vincent Banrey; Asst. Project Director, Catherine Whan; Editors (1986): Maricruz Saunders; (1987): Juan Jimenez, GloryAnn Torres; LAYOUT DESIGNERS: Vincent Banrey, Stephanie Bowen, Yvonne Brown, Jacqui Fernandez, Milton Ferreira, Omar Harris, Cornelius Huskins, Juan Jimenez, Wayne Keane, Richard Massie, Victoria Pamias, Richard Provost, Maricruz Saunders, GloryAnn Torres, Pedro Torres, Joan Walker, Catherine Whan. PHOTOGRAPHERS: John Carrero, Young Baek Choi, Randy Fader-Smith, Milton Ferreira, Roger Ince, Juan Jimenez, Umoja Kwanguvu, Seymour Lerman, Clinton Linton, Richard Provost, Jaidee amsinghani, Maricruz Saunders, Frank Tocco, GloryAnn Torres, Catherine Whan, Alan Young. ARTISTS: Cover Design: Madeline Vega; Endsheets: Oscar "DJ Ozzie" Ramirez; Division Pages: Jose Marti; International LaGuardia: Jacqui Fernandez; Illustrations: Richard Massie, Jacqui Fernandez, Madeline Vega. WRITERS: Yasmin Ahmed, Vincent Banrey, Warren Gardner, Juan Jimenez, Umoja Kwanguvu, Luis Merchant, Victoria Pamias, Richard Provost, Christiana Somerville, GloryAnn Torres, Joan Walker, Catherine Whan. SIGNIFICANT OTHERS: Word Processing: Blanca Arbito, Edward Hollins, Catherine Whan. Vincent Banrey Spread: developed by Blanca Arbito, Edward Hollins and GloryAnn Torres, Jacqui Fernandez, Catherine Whan. Creative Consultant: Edward Hollins. Promotions: George Condors. SPECIAL THANKS TO: Frank and Seymour of Classic Studios; Chuck Lindsey, Photo Workshop Instructor; Ted Schiffman of Taylor Publishing Co.; Dan Horn and Thurston Reyes of LaGuardia Theatre; and the Recreation staff. ALAN BERMAN IN MEMORIAM: Sketch, Tom Fink; Alan Speaking, Brian Gallagher; Remembering Dr. Alan Berman, Tuzyline Allan.
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Abyssal peridotites are normally thought to be residues of melting of the mid-ocean ridge basalt (MORB) source and are presumably a record of processes affecting the upper mantle. Samples from a single section of abyssal peridotite from the Kane Transform area in the Atlantic Ocean were examined for 190Pt-186Os and 187Re-187Os systematics. They have uniform 186Os/188Os ratios with a mean of 0.1198353 +/- 7, identical to the mean of 0.1198340 +/-12 for Os-Ir alloys and chromitites believed to be representative of the upper mantle. While the Pt/Os ratios of the upper mantle may be affected locally by magmatic processes, these data show that the Pt/Os ratio for the bulk upper mantle has not deviated by more than about +/- 30% from a chondritic Pt/Os ratio over 4.5 billion years. These observations are consistent with the addition of a chondritic late veneer after core separation as the primary control on the highly siderophile element budget of the terrestrial upper mantle. The 187Os/188Os of the samples range from 0.12267 to 0.12760 and correlate well with Pt and Pt/Os, but not Re/Os. These relationships may be explained by variable amounts of partial melting with changing D(Re), reflecting in part garnet in the residue, with a model-dependent melting age between about 600 and 1700 Ma. A model where the correlation between Pt/Os and 187Os/188Os results from multiple ancient melting events, in mantle peridotites that were later juxtaposed by convection, is also consistent with these data. This melting event or events are evidently unrelated to recent melting under mid-ocean ridges, because recent melting would have disturbed the relationship between Pt/Os and 187Os/188Os. Instead, this section of abyssal peridotite may be a block of refractory mantle that remained isolated from the convecting portions of the upper mantle for 600 Ma to >1 Ga. Alternatively, Pt and Os may have been sequestered during more recent melting and possibly melt/rock reaction processes, thereby preserving an ancient melting history. If representative of other abyssal peridotites, then the rocks from this suite with subchondritic 187Os/188Os are not simple residues of recent MORB source melting at ridges, but instead have a more complex history. This suite of variably depleted samples projects to an undepleted present-day Pt/Os of about 2.2 and 187Os/188Os of about 0.128-0.129, consistent with estimates for the primitive upper mantle.
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Mode of access: Internet.
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Mode of access: Internet.
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Mode of access: Internet.
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Mode of access: Internet.
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"Critical essay on authorities": p. [321]-333.
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v. I. Bks. I-XII -- v. II. Bks. XIII-XXIV, trans. by John Conington.
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Plates printed on both sides.
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"Extrait des Mémoires de la Société des antiquaires de Normandie."