Results 231 to 240 of about 220,882 (295)

Study on the genesis mechanism of geothermal resources in the Yunkai area, South China based on geophysical data. [PDF]

Sci Rep
Zhou Y, Qiu N, Zhu C, Liao K, Feng Q, Song J, Li K, Zhang Z.   +7 more
europepmc   +1 more source

Bridging the gap between subduction dynamics and the long-term strength of the Sunda megathrust. [PDF]

Nat Commun
Capitanio FA, Gollapalli T, Munukutla R, Graciosa JC, Mohd Z, Beall A, Dal Zilio L.   +6 more
europepmc   +1 more source

Onset of slab mantle melting in Earth's lower mantle: Evidence from ferropericlase in superdeep diamonds. [PDF]

Sci Adv
Ni P, Shirey SB, Walter MJ, Czas J, Novella D, Nestola F, Kueter N, Smith EM, Stachel T, Pearson DG, Steele A, Gardner LL, Jacobsen SD, Harte B, Harris JW, Shahar A.   +15 more
europepmc   +1 more source

Mantle-derived fluid flux controls Olympic Dam-style Fe oxide-Cu-Au mineralisation. [PDF]

Sci Rep
Thiel S, Reid A, Heinson G, Brand K, Li L.   +4 more
europepmc   +1 more source

The importance of past rifting in large igneous province development. [PDF]

Nature
Kounoudis R, Bastow ID, Ebinger CJ, Goes S, Zhou P, Musila M, Ogden CS, Ayele A.   +7 more
europepmc   +1 more source

Some of the next articles are maybe not open access.

Related searches:

Independent hydrogen incorporation in wadsleyite from oxygen fugacity and non-dissociation of H2O in the reducing mantle transition zone

Earth and Planetary Science Letters, 2021
The mantle transition zone is considered as a potential water reservoir in the Earth's interior because of the high H2O solubility in wadsleyite and ringwoodite.
Hongzhan Fei, Tomoo Katsura
exaly   +2 more sources

High water solubility of ringwoodite at mantle transition zone temperature

Earth and Planetary Science Letters, 2020
The mantle transition zone, a potential water reservoir in the Earth's interior, is suggested to contain more than 1 wt.% of H2O, at least locally, by the natural water-rich ringwoodite inclusion ( Pearson et al., 2014 ) and the mineral viscosity ( Fei ...
Hongzhan Fei, Tomoo Katsura
exaly   +2 more sources

Variability of subducting slab morphologies in the mantle transition zone: Insight from petrological-thermomechanical modeling

Earth-Science Reviews, 2019
Variable morphologies of subducting slabs are observed in tomographic images of the mantle transition zone (MTZ), where slabs appear to stagnate in the MTZ or enter the lower mantle. These contrasting morphologies of subducting slabs are dependent on the
Zhong-Hai Li, Taras Gerya, James A D Connolly   +2 more
exaly   +2 more sources

Seismic evidence for water transport out of the mantle transition zone beneath the European Alps

Earth and Planetary Science Letters, 2018
Zhen Liu, Jeffrey Park, Shun-Ichiro Karato   +2 more
exaly   +2 more sources

Nephelinites in eastern China originating from the mantle transition zone

, 2021
Nephelinites, a highly alkaline volcanic rock type, have widely been thought to be formed in a shallow lithosphere previously impregnated with phlogopite and/or amphibole.
G. Zeng, Li‐Hui Chen, A. Hofmann, Xiao‐Jun Wang, Jian‐Qiang Liu, Xun Yu, Liewen Xie   +6 more
semanticscholar   +1 more source