Raman spectroscopic analysis of carbonaceous matter and silica in the test walls of recent and fossil agglutinated foraminifera (Record no. 191349)

MARC details
000 -LEADER
fixed length control field 02540nab a2200229 4500
008 - CÓDIGOS DE INFORMACIÓN DE LONGITUD FIJA - INFORMACIÓN GENERAL
Campo de control de longitud fija 260224s2015 xxu ing
041 ## - IDIOMA
Idioma Inglés
245 00 - TITULO
Título Raman spectroscopic analysis of carbonaceous matter and silica in the test walls of recent and fossil agglutinated foraminifera
260 ## - PUBLICACION, DISTRIBUCION, ETC
Lugar de publicación, distribución, etc.
Nombre de publicador, distribuidor, etc.
Fecha de publicación, distribución, etc. jun. 2015
270 ## - FECHA DE CARGA
Fecha de carga 17/10/2017 ; 17/10/2017
300 ## - DESCRIPCION FISICA
Otra extensión 16 p. ; 1081-1097
520 ## - RESUMEN, ETC
Resumen Transcripción del resumen del autor: Previous HitRamanNext Hit spectroscopy has been used extensively in thermal maturation studies of kerogen, but has not been used to examine the maturation of organic cements in agglutinated foraminifera. Here, we use Previous HitRamanNext Hit spectroscopy to document the existence of carbonaceous matter and silica in recent and fossil agglutinated foraminifera, and to measure thermal alteration effects in fossil foraminifera. The distribution of carbonaceous matter through the test (shell) walls of agglutinated foraminifera suggests that this carbonaceous material is derived from primary organic cement and not from random contamination. Fossil specimens exhibit three broad stages of maturation: (1) Immature specimens are characterized by moderately strong fluorescence, broad, low intensity Previous HitRamanNext Hit peaks (relative to fluorescence), and a tendency for the G-band to occur at lower wave numbers. These attributes are consistent with the presence of amorphous carbonaceous matter and minor organic degradation. (2) Mature samples (oil window) exhibit high fluorescence, increased relative D- and G-band intensities, and a decreased width of the D-band. (3) Postmature samples exhibit low levels of fluorescence and high relative D- and G-band intensities, a tendency for the G-band to be located at higher wave numbers, an increase in the D:G band ratio, and an increase of the relative intensity of the silica peak. This stage is consistent with the presence of highly ordered carbonaceous matter and diagenetic quartz. These findings indicate that Previous HitRamanNext Hit Previous HitspectroscopicTop analysis of fossil agglutinated foraminifera can be used as a quick and easy tool to assess thermal maturity and estimate optimal temperatures for hydrocarbon generation.
581 ## - ESTADO DE COLECCIÓN
Estado de colección 6
773 0# - CORRECCIÓN
Título AAPG Bulletin
Partes relacionadas
942 ## - DESC. DE MATERIAL
Tipo de item KOHA Artículo de Revista
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre McNeil, David H.
9 (RLIN) 57369
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Schulze, H. Georg
9 (RLIN) 57370
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Matys, Emily
9 (RLIN) 57371
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Bosak, Tanja
9 (RLIN) 57372
Holdings
Biblioteca propietaria Biblioteca actual Fecha de adquisición Inventario Total de préstamos Inventario Fecha de carga Tipo de item KOHA
Biblioteca Alejandro Angel Bulgheroni Biblioteca Alejandro Angel Bulgheroni 06/03/2026 200063624   200063624 06/03/2026 Artículo de Revista


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