التفاصيل البيبلوغرافية
العنوان: |
(Table 4) Magnetic properties of titanomagnetite in MORB younger than 100 Ma, DSDP Hole 63-469 |
المؤلفون: |
Wang, Daming, Van der Voo, Rob, Peacor, Donald R |
بيانات النشر: |
PANGAEA |
سنة النشر: |
2005 |
المجموعة: |
PANGAEA - Data Publisher for Earth & Environmental Science (AWI Bremerhaven / MARUM Bremen) |
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 |
نوع الوثيقة: |
dataset |
وصف الملف: |
text/tab-separated-values, 32 data points |
اللغة: |
English |
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 |
DOI: |
10.1594/PANGAEA.711513 |
الإتاحة: |
https://doi.org/10.1594/PANGAEA.711513Test https://doi.org/10.1594/PANGAEA.711520Test |
حقوق: |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported ; Access constraints: unrestricted ; info:eu-repo/semantics/openAccess |
رقم الانضمام: |
edsbas.B15CCD87 |
قاعدة البيانات: |
BASE |