Water-rich sublithospheric melt channel in the equatorial Atlantic Ocean
The lithosphere–asthenosphere boundary is the most extensive boundary on Earth, separating the mobile plate above from the convecting mantle below, but its nature remains a matter of debate. Using an ultra-deep seismic reflection technique, here we show a systematic seismic image of two deep reflect...
Saved in:
Main Authors: | Mehouachi, Fares, Singh, Satish C. |
---|---|
Other Authors: | Earth Observatory of Singapore |
Format: | Article |
Language: | English |
Published: |
2020
|
Subjects: | |
Online Access: | https://hdl.handle.net/10356/143768 |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Institution: | Nanyang Technological University |
Language: | English |
Similar Items
-
Episodic kinematics in continental rifts modulated by changes in mantle melt fraction
by: Moore, James Daniel Paul, et al.
Published: (2017) -
Seismic structure of the upper crust from 0-75 Ma in the equatorial Atlantic Ocean on the African plate using ultralong offset seismic data
by: Audhkhasi, P., et al.
Published: (2021) -
Pemanfaatan Data Pengamatan GNSS Stasiun Sugar (Sumatran GPS Array) dan Ina-CORS (Indonesian Continously Operating Reference Station) untuk Estimasi Nilai dan Pola Regangan Tektonik dalam Bentuk Grid di Patahan Sumatra Tahun 2012-2013
by: Riyadi, Gondang, et al.
Published: (2016) -
Adjoint traveltime tomography unravels a scenario of horizontal mantle flow beneath the North China craton
by: Dong, Xingpeng, et al.
Published: (2021) -
Long-lived shallow slow-slip events on the Sunda megathrust
by: Mallick, Rishav, et al.
Published: (2021)