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...

Бүрэн тодорхойлолт

Номзүйн дэлгэрэнгүй
Үндсэн зохиолчид: Lissenberg, C. Johan, Rioux, Matthew, MacLeod, Christopher J., Shimizu, Nobumichi, Bowring, Samuel A.
Бусад зохиолчид: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Формат: Өгүүллэг
Хэл сонгох:en_US
Хэвлэсэн: American Geophysical Union (AGU) 2017
Онлайн хандалт:http://hdl.handle.net/1721.1/106330
https://orcid.org/0000-0001-9722-469X