(Table 4) Magnetic properties of titanomagnetite in MORB younger than 100 Ma, DSDP Hole 49-412A

Bibliographic Details
Main Authors: Wang, Daming, Van der Voo, Rob, Peacor, Donald R
Format: Dataset
Language:English
Published: PANGAEA 2005
Subjects:
49-412A
AGE
Coercivity
Curie temperature
Deep Sea Drilling Project
DEPTH
sediment/rock
DRILL
Drilling/drill rig
DSDP
DSDP/ODP/IODP sample designation
Glomar Challenger
Hysteresis
coercivity of remanence/coercivity
saturation magnetization/ saturation remanence
saturation remanence
Leg49
Natural remanent magnetization
Intensity per unit mass
North Atlantic/FRACTURE ZONE
Sample code/label
vibrating sample magnetometer (microVSM)
North Atlantic
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.711510
https://doi.org/10.1594/PANGAEA.711510
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.711510
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.711510 2023-05-15T17:30:47+02:00 (Table 4) Magnetic properties of titanomagnetite in MORB younger than 100 Ma, DSDP Hole 49-412A Wang, Daming Van der Voo, Rob Peacor, Donald R LATITUDE: 36.562300 * LONGITUDE: -33.166000 * DATE/TIME START: 1976-08-24T00:00:00 * DATE/TIME END: 1976-08-24T00:00:00 * MINIMUM DEPTH, sediment/rock: 176.73 m * MAXIMUM DEPTH, sediment/rock: 282.91 m 2005-01-20 text/tab-separated-values, 21 data points https://doi.pangaea.de/10.1594/PANGAEA.711510 https://doi.org/10.1594/PANGAEA.711510 en eng PANGAEA https://doi.org/10.1594/PANGAEA.711520 Wang, Daming; Van der Voo, Rob; Peacor, Donald R (2005): Why is the remanent magnetic intensity of Cretaceous MORB so much higher than that of mid to late Cenozoic MORB? Geosphere, 1(3), 138-146, https://doi.org/10.1130/GES00024.1 https://doi.pangaea.de/10.1594/PANGAEA.711510 https://doi.org/10.1594/PANGAEA.711510 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY 49-412A AGE Coercivity Curie temperature Deep Sea Drilling Project DEPTH sediment/rock DRILL Drilling/drill rig DSDP DSDP/ODP/IODP sample designation Glomar Challenger Hysteresis coercivity of remanence/coercivity saturation magnetization/ saturation remanence saturation remanence Leg49 Natural remanent magnetization Intensity per unit mass North Atlantic/FRACTURE ZONE Sample code/label vibrating sample magnetometer (microVSM) Dataset 2005 ftpangaea https://doi.org/10.1594/PANGAEA.711510 https://doi.org/10.1594/PANGAEA.711520 2023-01-20T09:34:27Z Dataset North Atlantic PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-33.166000,-33.166000,36.562300,36.562300)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic 49-412A
AGE
Coercivity
Curie temperature
Deep Sea Drilling Project
DEPTH
sediment/rock
DRILL
Drilling/drill rig
DSDP
DSDP/ODP/IODP sample designation
Glomar Challenger
Hysteresis
coercivity of remanence/coercivity
saturation magnetization/ saturation remanence
saturation remanence
Leg49
Natural remanent magnetization
Intensity per unit mass
North Atlantic/FRACTURE ZONE
Sample code/label
vibrating sample magnetometer (microVSM)
spellingShingle 49-412A
AGE
Coercivity
Curie temperature
Deep Sea Drilling Project
DEPTH
sediment/rock
DRILL
Drilling/drill rig
DSDP
DSDP/ODP/IODP sample designation
Glomar Challenger
Hysteresis
coercivity of remanence/coercivity
saturation magnetization/ saturation remanence
saturation remanence
Leg49
Natural remanent magnetization
Intensity per unit mass
North Atlantic/FRACTURE ZONE
Sample code/label
vibrating sample magnetometer (microVSM)
Wang, Daming
Van der Voo, Rob
Peacor, Donald R
(Table 4) Magnetic properties of titanomagnetite in MORB younger than 100 Ma, DSDP Hole 49-412A
topic_facet 49-412A
AGE
Coercivity
Curie temperature
Deep Sea Drilling Project
DEPTH
sediment/rock
DRILL
Drilling/drill rig
DSDP
DSDP/ODP/IODP sample designation
Glomar Challenger
Hysteresis
coercivity of remanence/coercivity
saturation magnetization/ saturation remanence
saturation remanence
Leg49
Natural remanent magnetization
Intensity per unit mass
North Atlantic/FRACTURE ZONE
Sample code/label
vibrating sample magnetometer (microVSM)
format Dataset
author Wang, Daming
Van der Voo, Rob
Peacor, Donald R
author_facet Wang, Daming
Van der Voo, Rob
Peacor, Donald R
author_sort Wang, Daming
title (Table 4) Magnetic properties of titanomagnetite in MORB younger than 100 Ma, DSDP Hole 49-412A
title_short (Table 4) Magnetic properties of titanomagnetite in MORB younger than 100 Ma, DSDP Hole 49-412A
title_full (Table 4) Magnetic properties of titanomagnetite in MORB younger than 100 Ma, DSDP Hole 49-412A
title_fullStr (Table 4) Magnetic properties of titanomagnetite in MORB younger than 100 Ma, DSDP Hole 49-412A
title_full_unstemmed (Table 4) Magnetic properties of titanomagnetite in MORB younger than 100 Ma, DSDP Hole 49-412A
title_sort (table 4) magnetic properties of titanomagnetite in morb younger than 100 ma, dsdp hole 49-412a
publisher PANGAEA
publishDate 2005
url https://doi.pangaea.de/10.1594/PANGAEA.711510
https://doi.org/10.1594/PANGAEA.711510
op_coverage LATITUDE: 36.562300 * LONGITUDE: -33.166000 * DATE/TIME START: 1976-08-24T00:00:00 * DATE/TIME END: 1976-08-24T00:00:00 * MINIMUM DEPTH, sediment/rock: 176.73 m * MAXIMUM DEPTH, sediment/rock: 282.91 m
long_lat ENVELOPE(-33.166000,-33.166000,36.562300,36.562300)
genre North Atlantic
genre_facet North Atlantic
op_relation https://doi.org/10.1594/PANGAEA.711520
Wang, Daming; Van der Voo, Rob; Peacor, Donald R (2005): Why is the remanent magnetic intensity of Cretaceous MORB so much higher than that of mid to late Cenozoic MORB? Geosphere, 1(3), 138-146, https://doi.org/10.1130/GES00024.1
https://doi.pangaea.de/10.1594/PANGAEA.711510
https://doi.org/10.1594/PANGAEA.711510
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.711510
https://doi.org/10.1594/PANGAEA.711520
_version_ 1766127803293499392

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