Crystallization depth beneath an oceanic detachment fault (ODP Hole 923A, Mid-Atlantic Ridge)
Oceanic detachment faults are increasingly recognized as playing an integral role in the seafloor spreading process at slow and ultraslow spreading mid-ocean ridges, with significant consequences for the architecture of the oceanic lithosphere. Although melt supply is considered to play a critical c...
| Үндсэн зохиолчид: | , , , , |
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| Бусад зохиолчид: | |
| Формат: | Өгүүллэг |
| Хэл сонгох: | en_US |
| Хэвлэсэн: |
American Geophysical Union (AGU)
2017
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| Онлайн хандалт: | http://hdl.handle.net/1721.1/106330 https://orcid.org/0000-0001-9722-469X |