(Table 2) Geochemistry of K-feldspars and associated plagioclase phenocrysts and rims at DSDP Legs 69, 52, 51 and 19
Basalts from some holes of the Deep Sea Drilling Project contain secondary K-feldspar which forms pseudomorphs after calcic (>76% An) Plagioclase cores, whereas Plagioclase of rims and microlites (68-74% An) remains unaltered. In basalts of Hole 504B two such grains with relics of Plagioclase in...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.816468 2023-05-15T17:35:23+02:00 (Table 2) Geochemistry of K-feldspars and associated plagioclase phenocrysts and rims at DSDP Legs 69, 52, 51 and 19 Pertsev, Nikolay N Boronikhin, V A MEDIAN LATITUDE: 21.260440 * MEDIAN LONGITUDE: -99.780720 * SOUTH-BOUND LATITUDE: 1.227200 * WEST-BOUND LONGITUDE: 164.713500 * NORTH-BOUND LATITUDE: 53.009500 * EAST-BOUND LONGITUDE: -68.041300 * DATE/TIME START: 1971-08-30T00:00:00 * DATE/TIME END: 1979-10-07T00:00:00 * MINIMUM ELEVATION: -5511.0 m * MAXIMUM ELEVATION: -3014.0 m 1983-07-09 text/tab-separated-values, 249 data points https://doi.pangaea.de/10.1594/PANGAEA.816468 https://doi.org/10.1594/PANGAEA.816468 en eng PANGAEA Pertsev, Nikolay N; Rusinov, V L (1980): Mineral assemblages and processes of alterations in basalts at Deep Sea Drilling Project Sites 417 and 418. In: Donnelly, T; Francheteau, J; Bryan, W; Robinson, P; Flower, M; Salisbury, M; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 51-53, 1219-1242, https://doi.org/10.2973/dsdp.proc.515253.148.1980 Stewart, Richard J; Natland, James H; Glassley, William R (1973): Petrology of volcanic rocks recovered on DSDP Leg 19 from the North Pacific Ocean and the Bering Sea. In: Creager, JS; Scholl, DW; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Government Print Office), 19, 615-627, https://doi.org/10.2973/dsdp.proc.19.114.1973 https://doi.pangaea.de/10.1594/PANGAEA.816468 https://doi.org/10.1594/PANGAEA.816468 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Pertsev, Nikolay N; Boronikhin, V A (1983): Secondary K-feldspar in basalts at Deep Sea Drilling Project Hole 504B and the problem of K-feldspathization in oceanic basalts. In: Cann, JR; Langseth, MG; Honnorez, J; Von Herzen, RP; White, SM; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 69, 589-591, https://doi.org/10.2973/dsdp.proc.69.132.1983 19-192A 51-417 52-418A 69-504B 69-505B Albite Aluminium oxide Anorthite Calcium oxide Calculated Deep Sea Drilling Project DRILL Drilling/drill rig DSDP DSDP/ODP/IODP sample designation Electron microprobe (EMP) Elevation of event Event label Glomar Challenger Latitude of event Leg19 Leg51 Leg52 Leg69 Longitude of event Minerals North Atlantic/CONT RISE North Pacific/GRABEN North Pacific/GUYOT Orthoclase Piece Potassium oxide Reference/source Sample code/label Sample ID Silicon dioxide Sodium oxide Total Dataset 1983 ftpangaea https://doi.org/10.1594/PANGAEA.816468 https://doi.org/10.2973/dsdp.proc.69.132.1983 https://doi.org/10.2973/dsdp.proc.515253.148.1980 https://doi.org/10.2973/dsdp.proc.19.114.1973 2023-01-20T09:01:18Z Basalts from some holes of the Deep Sea Drilling Project contain secondary K-feldspar which forms pseudomorphs after calcic (>76% An) Plagioclase cores, whereas Plagioclase of rims and microlites (68-74% An) remains unaltered. In basalts of Hole 504B two such grains with relics of Plagioclase in the central parts of phenocysts were recovered. The composition of the Plagioclase rims and of non-replaced phenocrysts is An79-81; the composition of relics is An83. The An and Ab contents of the K-feldspar is higher than in K-feldspar from altered basalt in Hole 418A in the Atlantic Ocean near the Bermuda Rise. Replacement of plagioclases by K-feldspar evidently is caused by oxygen-rich nearbottom sea water penetrating into basalts. The temperature interval of K-feldspathization is probably in the range 30 to 80°C, more-calcic Plagioclase being replaced by K-feldspar at higher temperatures. Dataset North Atlantic PANGAEA - Data Publisher for Earth & Environmental Science Pacific ENVELOPE(164.713500,-68.041300,53.009500,1.227200) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
19-192A 51-417 52-418A 69-504B 69-505B Albite Aluminium oxide Anorthite Calcium oxide Calculated Deep Sea Drilling Project DRILL Drilling/drill rig DSDP DSDP/ODP/IODP sample designation Electron microprobe (EMP) Elevation of event Event label Glomar Challenger Latitude of event Leg19 Leg51 Leg52 Leg69 Longitude of event Minerals North Atlantic/CONT RISE North Pacific/GRABEN North Pacific/GUYOT Orthoclase Piece Potassium oxide Reference/source Sample code/label Sample ID Silicon dioxide Sodium oxide Total |
spellingShingle |
19-192A 51-417 52-418A 69-504B 69-505B Albite Aluminium oxide Anorthite Calcium oxide Calculated Deep Sea Drilling Project DRILL Drilling/drill rig DSDP DSDP/ODP/IODP sample designation Electron microprobe (EMP) Elevation of event Event label Glomar Challenger Latitude of event Leg19 Leg51 Leg52 Leg69 Longitude of event Minerals North Atlantic/CONT RISE North Pacific/GRABEN North Pacific/GUYOT Orthoclase Piece Potassium oxide Reference/source Sample code/label Sample ID Silicon dioxide Sodium oxide Total Pertsev, Nikolay N Boronikhin, V A (Table 2) Geochemistry of K-feldspars and associated plagioclase phenocrysts and rims at DSDP Legs 69, 52, 51 and 19 |
topic_facet |
19-192A 51-417 52-418A 69-504B 69-505B Albite Aluminium oxide Anorthite Calcium oxide Calculated Deep Sea Drilling Project DRILL Drilling/drill rig DSDP DSDP/ODP/IODP sample designation Electron microprobe (EMP) Elevation of event Event label Glomar Challenger Latitude of event Leg19 Leg51 Leg52 Leg69 Longitude of event Minerals North Atlantic/CONT RISE North Pacific/GRABEN North Pacific/GUYOT Orthoclase Piece Potassium oxide Reference/source Sample code/label Sample ID Silicon dioxide Sodium oxide Total |
description |
Basalts from some holes of the Deep Sea Drilling Project contain secondary K-feldspar which forms pseudomorphs after calcic (>76% An) Plagioclase cores, whereas Plagioclase of rims and microlites (68-74% An) remains unaltered. In basalts of Hole 504B two such grains with relics of Plagioclase in the central parts of phenocysts were recovered. The composition of the Plagioclase rims and of non-replaced phenocrysts is An79-81; the composition of relics is An83. The An and Ab contents of the K-feldspar is higher than in K-feldspar from altered basalt in Hole 418A in the Atlantic Ocean near the Bermuda Rise. Replacement of plagioclases by K-feldspar evidently is caused by oxygen-rich nearbottom sea water penetrating into basalts. The temperature interval of K-feldspathization is probably in the range 30 to 80°C, more-calcic Plagioclase being replaced by K-feldspar at higher temperatures. |
format |
Dataset |
author |
Pertsev, Nikolay N Boronikhin, V A |
author_facet |
Pertsev, Nikolay N Boronikhin, V A |
author_sort |
Pertsev, Nikolay N |
title |
(Table 2) Geochemistry of K-feldspars and associated plagioclase phenocrysts and rims at DSDP Legs 69, 52, 51 and 19 |
title_short |
(Table 2) Geochemistry of K-feldspars and associated plagioclase phenocrysts and rims at DSDP Legs 69, 52, 51 and 19 |
title_full |
(Table 2) Geochemistry of K-feldspars and associated plagioclase phenocrysts and rims at DSDP Legs 69, 52, 51 and 19 |
title_fullStr |
(Table 2) Geochemistry of K-feldspars and associated plagioclase phenocrysts and rims at DSDP Legs 69, 52, 51 and 19 |
title_full_unstemmed |
(Table 2) Geochemistry of K-feldspars and associated plagioclase phenocrysts and rims at DSDP Legs 69, 52, 51 and 19 |
title_sort |
(table 2) geochemistry of k-feldspars and associated plagioclase phenocrysts and rims at dsdp legs 69, 52, 51 and 19 |
publisher |
PANGAEA |
publishDate |
1983 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.816468 https://doi.org/10.1594/PANGAEA.816468 |
op_coverage |
MEDIAN LATITUDE: 21.260440 * MEDIAN LONGITUDE: -99.780720 * SOUTH-BOUND LATITUDE: 1.227200 * WEST-BOUND LONGITUDE: 164.713500 * NORTH-BOUND LATITUDE: 53.009500 * EAST-BOUND LONGITUDE: -68.041300 * DATE/TIME START: 1971-08-30T00:00:00 * DATE/TIME END: 1979-10-07T00:00:00 * MINIMUM ELEVATION: -5511.0 m * MAXIMUM ELEVATION: -3014.0 m |
long_lat |
ENVELOPE(164.713500,-68.041300,53.009500,1.227200) |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Supplement to: Pertsev, Nikolay N; Boronikhin, V A (1983): Secondary K-feldspar in basalts at Deep Sea Drilling Project Hole 504B and the problem of K-feldspathization in oceanic basalts. In: Cann, JR; Langseth, MG; Honnorez, J; Von Herzen, RP; White, SM; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 69, 589-591, https://doi.org/10.2973/dsdp.proc.69.132.1983 |
op_relation |
Pertsev, Nikolay N; Rusinov, V L (1980): Mineral assemblages and processes of alterations in basalts at Deep Sea Drilling Project Sites 417 and 418. In: Donnelly, T; Francheteau, J; Bryan, W; Robinson, P; Flower, M; Salisbury, M; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 51-53, 1219-1242, https://doi.org/10.2973/dsdp.proc.515253.148.1980 Stewart, Richard J; Natland, James H; Glassley, William R (1973): Petrology of volcanic rocks recovered on DSDP Leg 19 from the North Pacific Ocean and the Bering Sea. In: Creager, JS; Scholl, DW; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Government Print Office), 19, 615-627, https://doi.org/10.2973/dsdp.proc.19.114.1973 https://doi.pangaea.de/10.1594/PANGAEA.816468 https://doi.org/10.1594/PANGAEA.816468 |
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.816468 https://doi.org/10.2973/dsdp.proc.69.132.1983 https://doi.org/10.2973/dsdp.proc.515253.148.1980 https://doi.org/10.2973/dsdp.proc.19.114.1973 |
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1766134544555048960 |