Vertically extensive and unstable magmatic systems: A unified view of igneous processes.
about
Platinum-bearing chromite layers are caused by pressure reduction during magma ascent.Geomorphic expression of rapid Holocene silicic magma reservoir growth beneath Laguna del Maule, Chile.Gravity modeling finds a large magma body in the deep crust below the Gulf of Naples, Italy.Geophysics From Terrestrial Time-Variable Gravity Measurements
P2860
Vertically extensive and unstable magmatic systems: A unified view of igneous processes.
description
2017 nî lūn-bûn
@nan
2017年の論文
@ja
2017年論文
@yue
2017年論文
@zh-hant
2017年論文
@zh-hk
2017年論文
@zh-mo
2017年論文
@zh-tw
2017年论文
@wuu
2017年论文
@zh
2017年论文
@zh-cn
name
Vertically extensive and unstable magmatic systems: A unified view of igneous processes.
@en
Vertically extensive and unstable magmatic systems: A unified view of igneous processes.
@nl
type
label
Vertically extensive and unstable magmatic systems: A unified view of igneous processes.
@en
Vertically extensive and unstable magmatic systems: A unified view of igneous processes.
@nl
prefLabel
Vertically extensive and unstable magmatic systems: A unified view of igneous processes.
@en
Vertically extensive and unstable magmatic systems: A unified view of igneous processes.
@nl
P356
P1433
P1476
Vertically extensive and unstable magmatic systems: A unified view of igneous processes.
@en
P2093
Jonathan D Blundy
P356
10.1126/SCIENCE.AAG3055
P407
P577
2017-03-01T00:00:00Z