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1
المؤلفون: Wang, Daming, Van der Voo, Rob, Peacor, Donald R
مصطلحات موضوعية: 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, Leg82, Natural remanent magnetization, Intensity per unit mass, North Atlantic/RIDGE, Sample code/label, vibrating sample magnetometer (microVSM)
جغرافية الموضوع: LATITUDE: 33.739300 * LONGITUDE: -43.767200 * DATE/TIME START: 1981-10-28T00:00:00 * DATE/TIME END: 1981-10-28T00:00:00 * MINIMUM DEPTH, sediment/rock: 286.07 m * MAXIMUM DEPTH, sediment/rock: 358.90 m
الوقت: 82-564
وصف الملف: text/tab-separated-values, 33 data points
العلاقة: https://doi.org/10.1594/PANGAEA.711520Test; 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/GES00024.1Test; https://doi.pangaea.de/10.1594/PANGAEA.711519Test; https://doi.org/10.1594/PANGAEA.711519Test
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2
المؤلفون: Wang, Daming, Van der Voo, Rob, Peacor, Donald R
مصطلحات موضوعية: 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, Leg82, Natural remanent magnetization, Intensity per unit mass, North Atlantic/RIDGE, Sample code/label, vibrating sample magnetometer (microVSM)
جغرافية الموضوع: LATITUDE: 33.141500 * LONGITUDE: -41.679300 * DATE/TIME START: 1981-10-21T00:00:00 * DATE/TIME END: 1981-10-21T00:00:00 * MINIMUM DEPTH, sediment/rock: 241.68 m * MAXIMUM DEPTH, sediment/rock: 315.71 m
الوقت: 82-562
وصف الملف: text/tab-separated-values, 37 data points
العلاقة: https://doi.org/10.1594/PANGAEA.711520Test; 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/GES00024.1Test; https://doi.pangaea.de/10.1594/PANGAEA.711518Test; https://doi.org/10.1594/PANGAEA.711518Test
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3
المؤلفون: Wang, Daming, Van der Voo, Rob, Peacor, Donald R
مصطلحات موضوعية: 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, Leg67, Natural remanent magnetization, Intensity per unit mass, North Pacific/TRENCH, Sample code/label, vibrating sample magnetometer (microVSM)
جغرافية الموضوع: LATITUDE: 12.496300 * LONGITUDE: -91.037700 * DATE/TIME START: 1979-05-26T00:00:00 * DATE/TIME END: 1979-05-26T00:00:00 * MINIMUM DEPTH, sediment/rock: 428.54 m * MAXIMUM DEPTH, sediment/rock: 441.14 m
الوقت: 67-495
وصف الملف: text/tab-separated-values, 25 data points
العلاقة: https://doi.org/10.1594/PANGAEA.711520Test; 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/GES00024.1Test; https://doi.pangaea.de/10.1594/PANGAEA.711515Test; https://doi.org/10.1594/PANGAEA.711515Test
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4
المؤلفون: Wang, Daming, Van der Voo, Rob, Peacor, Donald R
مصطلحات موضوعية: 72-516F, 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, Leg72, Natural remanent magnetization, Intensity per unit mass, Sample code/label, South Atlantic/CONT RISE, vibrating sample magnetometer (microVSM)
جغرافية الموضوع: LATITUDE: -30.276500 * LONGITUDE: -35.285000 * DATE/TIME START: 1980-03-11T00:00:00 * DATE/TIME END: 1980-03-11T00:00:00 * MINIMUM DEPTH, sediment/rock: 1263.36 m * MAXIMUM DEPTH, sediment/rock: 1269.89 m
وصف الملف: text/tab-separated-values, 13 data points
العلاقة: https://doi.org/10.1594/PANGAEA.711520Test; 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/GES00024.1Test; https://doi.pangaea.de/10.1594/PANGAEA.711516Test; https://doi.org/10.1594/PANGAEA.711516Test
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5
المؤلفون: Wang, Daming, Van der Voo, Rob, Peacor, Donald R
مصطلحات موضوعية: 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, Leg63, Natural remanent magnetization, Intensity per unit mass, North Pacific/ESCARPMENT, Sample code/label, vibrating sample magnetometer (microVSM)
جغرافية الموضوع: LATITUDE: 32.616700 * LONGITUDE: -120.548300 * DATE/TIME START: 1978-10-27T00:00:00 * DATE/TIME END: 1978-10-27T00:00:00 * MINIMUM DEPTH, sediment/rock: 382.88 m * MAXIMUM DEPTH, sediment/rock: 451.08 m
الوقت: 63-469
وصف الملف: text/tab-separated-values, 32 data points
العلاقة: https://doi.org/10.1594/PANGAEA.711520Test; 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/GES00024.1Test; https://doi.pangaea.de/10.1594/PANGAEA.711513Test; https://doi.org/10.1594/PANGAEA.711513Test
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6
المؤلفون: Wang, Daming, Van der Voo, Rob, Peacor, Donald R
مصطلحات موضوعية: 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, Leg54, Natural remanent magnetization, Intensity per unit mass, North Pacific/TROUGH, Sample code/label, vibrating sample magnetometer (microVSM)
جغرافية الموضوع: LATITUDE: 8.113200 * LONGITUDE: -104.605800 * DATE/TIME START: 1977-06-04T00:00:00 * DATE/TIME END: 1977-06-04T00:00:00 * MINIMUM DEPTH, sediment/rock: 150.00 m * MAXIMUM DEPTH, sediment/rock: 161.77 m
الوقت: 54-427
وصف الملف: text/tab-separated-values, 20 data points
العلاقة: https://doi.org/10.1594/PANGAEA.711520Test; 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/GES00024.1Test; https://doi.pangaea.de/10.1594/PANGAEA.711511Test; https://doi.org/10.1594/PANGAEA.711511Test
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7
المؤلفون: Wang, Daming, Van der Voo, Rob, Peacor, Donald R
مصطلحات موضوعية: 78-543A, 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, Leg78, Leg78AB, Natural remanent magnetization, Intensity per unit mass, North Atlantic/CONT RISE, Sample code/label, vibrating sample magnetometer (microVSM)
جغرافية الموضوع: LATITUDE: 15.712300 * LONGITUDE: -58.653700 * DATE/TIME START: 1981-02-28T00:00:00 * DATE/TIME END: 1981-02-28T00:00:00 * MINIMUM DEPTH, sediment/rock: 409.20 m * MAXIMUM DEPTH, sediment/rock: 448.40 m
وصف الملف: text/tab-separated-values, 32 data points
العلاقة: https://doi.org/10.1594/PANGAEA.711520Test; 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/GES00024.1Test; https://doi.pangaea.de/10.1594/PANGAEA.711517Test; https://doi.org/10.1594/PANGAEA.711517Test
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8
المؤلفون: Wang, Daming, Van der Voo, Rob, Peacor, Donald R
مصطلحات موضوعية: 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, Leg58, Natural remanent magnetization, Intensity per unit mass, North Pacific/Philippine Sea/BASIN, Sample code/label, vibrating sample magnetometer (microVSM)
جغرافية الموضوع: LATITUDE: 24.700700 * LONGITUDE: 132.774800 * DATE/TIME START: 1978-01-18T00:00:00 * DATE/TIME END: 1978-01-18T00:00:00 * MINIMUM DEPTH, sediment/rock: 395.85 m * MAXIMUM DEPTH, sediment/rock: 420.27 m
الوقت: 58-446
وصف الملف: text/tab-separated-values, 20 data points
العلاقة: https://doi.org/10.1594/PANGAEA.711520Test; 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/GES00024.1Test; https://doi.pangaea.de/10.1594/PANGAEA.711512Test; https://doi.org/10.1594/PANGAEA.711512Test
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9
المؤلفون: Wang, Daming, Van der Voo, Rob, Peacor, Donald R
مصطلحات موضوعية: 65-483B, 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, Leg65, Natural remanent magnetization, Intensity per unit mass, North Pacific/Gulf of California/CONT RISE, Sample code/label, vibrating sample magnetometer (microVSM)
جغرافية الموضوع: LATITUDE: 22.883200 * LONGITUDE: -108.747300 * DATE/TIME START: 1979-02-12T00:00:00 * DATE/TIME END: 1979-02-12T00:00:00 * MINIMUM DEPTH, sediment/rock: 122.35 m * MAXIMUM DEPTH, sediment/rock: 261.57 m
وصف الملف: text/tab-separated-values, 26 data points
العلاقة: https://doi.org/10.1594/PANGAEA.711520Test; 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/GES00024.1Test; https://doi.pangaea.de/10.1594/PANGAEA.711514Test; https://doi.org/10.1594/PANGAEA.711514Test
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10
المؤلفون: Wang, Daming, Van der Voo, Rob, Peacor, Donald R
مصطلحات موضوعية: 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)
جغرافية الموضوع: 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
وصف الملف: text/tab-separated-values, 21 data points
العلاقة: https://doi.org/10.1594/PANGAEA.711520Test; 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/GES00024.1Test; https://doi.pangaea.de/10.1594/PANGAEA.711510Test; https://doi.org/10.1594/PANGAEA.711510Test