Flows with 'Cu-type' characteristics at ODP Hole 104-642E (Table 1) ...

Native Cu occurs in amygdules, fractures and groundmass of tholeiites from Ocean Drilling Program Site 642 on the Vøring Plateau. Similar occurrences have been reported in other tholeiites of the early Tertiary North Atlantic Volcanic Province drilled at Deep Sea Drilling Project Sites 342 on the Vø...

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Bibliographic Details
Main Author: LeHuray, A P
Format: Dataset
Language:English
Published: PANGAEA 1989
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.737392
https://doi.pangaea.de/10.1594/PANGAEA.737392
id ftdatacite:10.1594/pangaea.737392
record_format openpolar
spelling ftdatacite:10.1594/pangaea.737392 2024-09-15T18:23:39+00:00 Flows with 'Cu-type' characteristics at ODP Hole 104-642E (Table 1) ... LeHuray, A P 1989 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.737392 https://doi.pangaea.de/10.1594/PANGAEA.737392 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.104.137.1989 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Sample code/label Sample code/label 2 Number Layer thickness Drilling/drill rig DSDP/ODP/IODP sample designation Leg104 Joides Resolution Ocean Drilling Program ODP dataset Supplementary Dataset Dataset 1989 ftdatacite https://doi.org/10.1594/pangaea.73739210.2973/odp.proc.sr.104.137.1989 2024-08-01T10:56:44Z Native Cu occurs in amygdules, fractures and groundmass of tholeiites from Ocean Drilling Program Site 642 on the Vøring Plateau. Similar occurrences have been reported in other tholeiites of the early Tertiary North Atlantic Volcanic Province drilled at Deep Sea Drilling Project Sites 342 on the Vøring Plateau and 553 on the Rockall Plateau. The flows containing the native Cu have distinctive alteration patterns characterized by the combination of reddened flow tops, distinctive pastel coloration of the upper parts of the flows, relative abundance of celadonite, and the presence of native Cu. These associations suggest that subaerial weathering and subsequent seawater-basalt interaction are related to the occurrence of native Cu. An additional factor may be the increase in compatibility of Cu in silicates and Fe- Ti oxides that may accompany sub-solidus oxidation of basaltic flows. Native Cu occurrences in Site 642 tholeiites have some striking similarities to the large native Cu deposits in the Precambrian ... : Supplement to: LeHuray, A P (1989): Native copper in ODP Site 642 theoleiites. In: Eldholm, O; Thiede, J; Taylor, E; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 104, 411-417 ... Dataset North Atlantic DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Sample code/label
Sample code/label 2
Number
Layer thickness
Drilling/drill rig
DSDP/ODP/IODP sample designation
Leg104
Joides Resolution
Ocean Drilling Program ODP
spellingShingle Sample code/label
Sample code/label 2
Number
Layer thickness
Drilling/drill rig
DSDP/ODP/IODP sample designation
Leg104
Joides Resolution
Ocean Drilling Program ODP
LeHuray, A P
Flows with 'Cu-type' characteristics at ODP Hole 104-642E (Table 1) ...
topic_facet Sample code/label
Sample code/label 2
Number
Layer thickness
Drilling/drill rig
DSDP/ODP/IODP sample designation
Leg104
Joides Resolution
Ocean Drilling Program ODP
description Native Cu occurs in amygdules, fractures and groundmass of tholeiites from Ocean Drilling Program Site 642 on the Vøring Plateau. Similar occurrences have been reported in other tholeiites of the early Tertiary North Atlantic Volcanic Province drilled at Deep Sea Drilling Project Sites 342 on the Vøring Plateau and 553 on the Rockall Plateau. The flows containing the native Cu have distinctive alteration patterns characterized by the combination of reddened flow tops, distinctive pastel coloration of the upper parts of the flows, relative abundance of celadonite, and the presence of native Cu. These associations suggest that subaerial weathering and subsequent seawater-basalt interaction are related to the occurrence of native Cu. An additional factor may be the increase in compatibility of Cu in silicates and Fe- Ti oxides that may accompany sub-solidus oxidation of basaltic flows. Native Cu occurrences in Site 642 tholeiites have some striking similarities to the large native Cu deposits in the Precambrian ... : Supplement to: LeHuray, A P (1989): Native copper in ODP Site 642 theoleiites. In: Eldholm, O; Thiede, J; Taylor, E; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 104, 411-417 ...
format Dataset
author LeHuray, A P
author_facet LeHuray, A P
author_sort LeHuray, A P
title Flows with 'Cu-type' characteristics at ODP Hole 104-642E (Table 1) ...
title_short Flows with 'Cu-type' characteristics at ODP Hole 104-642E (Table 1) ...
title_full Flows with 'Cu-type' characteristics at ODP Hole 104-642E (Table 1) ...
title_fullStr Flows with 'Cu-type' characteristics at ODP Hole 104-642E (Table 1) ...
title_full_unstemmed Flows with 'Cu-type' characteristics at ODP Hole 104-642E (Table 1) ...
title_sort flows with 'cu-type' characteristics at odp hole 104-642e (table 1) ...
publisher PANGAEA
publishDate 1989
url https://dx.doi.org/10.1594/pangaea.737392
https://doi.pangaea.de/10.1594/PANGAEA.737392
genre North Atlantic
genre_facet North Atlantic
op_relation https://dx.doi.org/10.2973/odp.proc.sr.104.137.1989
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.73739210.2973/odp.proc.sr.104.137.1989
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