Semiquantitative occurence of various minerals in sediment core CRP-2A
The mineralogy of the lower Oligocene to Quaternary sediments of core CRP-2/2A drilled on the continental shelf of McMurdo Sound in Ross Sea, Antarctica, was examined by the X-ray diffraction method. Quartz, plagioclase feldspar and K-feldspar are the most important non-clay minerals. Pyroxene and a...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.55616 2023-05-15T14:04:42+02:00 Semiquantitative occurence of various minerals in sediment core CRP-2A Neumann, M Ehrmann, Werner LATITUDE: -77.005980 * LONGITUDE: 163.719450 * DATE/TIME START: 1998-10-16T07:30:00 * DATE/TIME END: 1998-11-25T14:20:00 * MINIMUM DEPTH, sediment/rock: 7.11 m * MAXIMUM DEPTH, sediment/rock: 623.81 m 1999-08-23 text/tab-separated-values, 797 data points https://doi.pangaea.de/10.1594/PANGAEA.55616 https://doi.org/10.1594/PANGAEA.55616 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.55616 https://doi.org/10.1594/PANGAEA.55616 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Neumann, M; Ehrmann, Werner (2000): Mineralogy of sediments from CRP-2/2A, Victoria Land Basin, Antarctica as revealed by x-ray diffraction. Terra Antartica, 7(4), 575-580, hdl:10013/epic.28294.d001 14.2 km at 096° true from Cape Roberts Amphibole/standard ratio Cape Roberts Project Core wireline system CRP CRP-2 CRP-2A CWS DEPTH sediment/rock Feldspar/standard ratio Feldspar 3.18 Å (Plagioclase)/standard ratio Feldspar 3.24 Å (Kalifeldspar)/standard ratio Grain size sieving/settling tube Kalifeldspar/Plagioclase ratio off Cape Roberts Ross Sea Antarctica Opal-CT/standard ratio Pyroxene/standard ratio Quartz/Feldspar ratio Quartz/standard ratio Sampling/drilling from ice Sand X-ray diffraction (XRD) Zeolite/standard ratio Dataset 1999 ftpangaea https://doi.org/10.1594/PANGAEA.55616 2023-01-20T07:35:51Z The mineralogy of the lower Oligocene to Quaternary sediments of core CRP-2/2A drilled on the continental shelf of McMurdo Sound in Ross Sea, Antarctica, was examined by the X-ray diffraction method. Quartz, plagioclase feldspar and K-feldspar are the most important non-clay minerals. Pyroxene and amphibole occur in minor amounts throughout the core. The composition of the sediments points to an origin in the Transantarctic Mountains for the majority of the detrital components. There, the plutonic and metamorphic rocks of the basement, the sediments of the Beacon Supergroup and the volcanic rocks of the Ferrar Group could serve as possible source lithologies. The distribution of the detrital minerals reflects a long-term history of successive erosion and valley incision. During the deposition of the lower part of the core, the detrital minerals were probably mainly derived from the sediments of the Beacon Supergroup, as indicated by the high quartz but relatively low feldspar abundances. In the upper c. 350 m of the core, the influence of a source in the basement became stronger and results in lower quartz contents but increasing abundance of feldspar. Some diagenetic alteration of the sediments is indicated by the occurrence of zeolites below c. 320 mbsf and of opal-CT above c. 320 mbsf. Dataset Antarc* Antarctica McMurdo Sound Ross Sea PANGAEA - Data Publisher for Earth & Environmental Science Ross Sea McMurdo Sound Transantarctic Mountains Cape Roberts ENVELOPE(-70.467,-70.467,-68.950,-68.950) ENVELOPE(163.719450,163.719450,-77.005980,-77.005980) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
14.2 km at 096° true from Cape Roberts Amphibole/standard ratio Cape Roberts Project Core wireline system CRP CRP-2 CRP-2A CWS DEPTH sediment/rock Feldspar/standard ratio Feldspar 3.18 Å (Plagioclase)/standard ratio Feldspar 3.24 Å (Kalifeldspar)/standard ratio Grain size sieving/settling tube Kalifeldspar/Plagioclase ratio off Cape Roberts Ross Sea Antarctica Opal-CT/standard ratio Pyroxene/standard ratio Quartz/Feldspar ratio Quartz/standard ratio Sampling/drilling from ice Sand X-ray diffraction (XRD) Zeolite/standard ratio |
spellingShingle |
14.2 km at 096° true from Cape Roberts Amphibole/standard ratio Cape Roberts Project Core wireline system CRP CRP-2 CRP-2A CWS DEPTH sediment/rock Feldspar/standard ratio Feldspar 3.18 Å (Plagioclase)/standard ratio Feldspar 3.24 Å (Kalifeldspar)/standard ratio Grain size sieving/settling tube Kalifeldspar/Plagioclase ratio off Cape Roberts Ross Sea Antarctica Opal-CT/standard ratio Pyroxene/standard ratio Quartz/Feldspar ratio Quartz/standard ratio Sampling/drilling from ice Sand X-ray diffraction (XRD) Zeolite/standard ratio Neumann, M Ehrmann, Werner Semiquantitative occurence of various minerals in sediment core CRP-2A |
topic_facet |
14.2 km at 096° true from Cape Roberts Amphibole/standard ratio Cape Roberts Project Core wireline system CRP CRP-2 CRP-2A CWS DEPTH sediment/rock Feldspar/standard ratio Feldspar 3.18 Å (Plagioclase)/standard ratio Feldspar 3.24 Å (Kalifeldspar)/standard ratio Grain size sieving/settling tube Kalifeldspar/Plagioclase ratio off Cape Roberts Ross Sea Antarctica Opal-CT/standard ratio Pyroxene/standard ratio Quartz/Feldspar ratio Quartz/standard ratio Sampling/drilling from ice Sand X-ray diffraction (XRD) Zeolite/standard ratio |
description |
The mineralogy of the lower Oligocene to Quaternary sediments of core CRP-2/2A drilled on the continental shelf of McMurdo Sound in Ross Sea, Antarctica, was examined by the X-ray diffraction method. Quartz, plagioclase feldspar and K-feldspar are the most important non-clay minerals. Pyroxene and amphibole occur in minor amounts throughout the core. The composition of the sediments points to an origin in the Transantarctic Mountains for the majority of the detrital components. There, the plutonic and metamorphic rocks of the basement, the sediments of the Beacon Supergroup and the volcanic rocks of the Ferrar Group could serve as possible source lithologies. The distribution of the detrital minerals reflects a long-term history of successive erosion and valley incision. During the deposition of the lower part of the core, the detrital minerals were probably mainly derived from the sediments of the Beacon Supergroup, as indicated by the high quartz but relatively low feldspar abundances. In the upper c. 350 m of the core, the influence of a source in the basement became stronger and results in lower quartz contents but increasing abundance of feldspar. Some diagenetic alteration of the sediments is indicated by the occurrence of zeolites below c. 320 mbsf and of opal-CT above c. 320 mbsf. |
format |
Dataset |
author |
Neumann, M Ehrmann, Werner |
author_facet |
Neumann, M Ehrmann, Werner |
author_sort |
Neumann, M |
title |
Semiquantitative occurence of various minerals in sediment core CRP-2A |
title_short |
Semiquantitative occurence of various minerals in sediment core CRP-2A |
title_full |
Semiquantitative occurence of various minerals in sediment core CRP-2A |
title_fullStr |
Semiquantitative occurence of various minerals in sediment core CRP-2A |
title_full_unstemmed |
Semiquantitative occurence of various minerals in sediment core CRP-2A |
title_sort |
semiquantitative occurence of various minerals in sediment core crp-2a |
publisher |
PANGAEA |
publishDate |
1999 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.55616 https://doi.org/10.1594/PANGAEA.55616 |
op_coverage |
LATITUDE: -77.005980 * LONGITUDE: 163.719450 * DATE/TIME START: 1998-10-16T07:30:00 * DATE/TIME END: 1998-11-25T14:20:00 * MINIMUM DEPTH, sediment/rock: 7.11 m * MAXIMUM DEPTH, sediment/rock: 623.81 m |
long_lat |
ENVELOPE(-70.467,-70.467,-68.950,-68.950) ENVELOPE(163.719450,163.719450,-77.005980,-77.005980) |
geographic |
Ross Sea McMurdo Sound Transantarctic Mountains Cape Roberts |
geographic_facet |
Ross Sea McMurdo Sound Transantarctic Mountains Cape Roberts |
genre |
Antarc* Antarctica McMurdo Sound Ross Sea |
genre_facet |
Antarc* Antarctica McMurdo Sound Ross Sea |
op_source |
Supplement to: Neumann, M; Ehrmann, Werner (2000): Mineralogy of sediments from CRP-2/2A, Victoria Land Basin, Antarctica as revealed by x-ray diffraction. Terra Antartica, 7(4), 575-580, hdl:10013/epic.28294.d001 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.55616 https://doi.org/10.1594/PANGAEA.55616 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.55616 |
_version_ |
1766275946224025600 |