Results 41 to 50 of about 112,018 (347)
Plume‐Induced Subduction Initiation: Single‐Slab or Multi‐Slab Subduction?
Initiation of subduction following the impingement of a hot buoyant mantle plume is one of the few scenarios that allow breaking the lithosphere and recycling a stagnant lid without requiring any preexisting weak zones.
Marzieh Baes+3 more
doaj +1 more source
Altered Mantle Fabric Beneath the Mid‐Continent Rift
We present new, densely sampled shear‐wave splitting results from southern Minnesota and adjacent areas of neighboring states, sampling the southwestern limit of the Archean Superior Province and straddling the Proterozoic Mid‐Continent Rift (MCR).
A. W. Frederiksen+4 more
doaj +1 more source
Spatio‐temporal changes of upper mantle structure play a significant role in generating and maintaining surface topography. Although geophysical models of upper mantle structure have become increasingly refined, there is a paucity of geologic constraints
P. W. Ball+4 more
doaj +1 more source
The thermal state and interior structure of Mars [PDF]
©2018. American Geophysical UnionThe present‐day thermal state, interior structure, composition, and rheology of Mars can be constrained by comparing the results of thermal history calculations with geophysical, petrological, and geological observations.
Banerdt, W. B.+8 more
core +2 more sources
Geochemistry and tectonic development of Cenozoic magmatism in the Carpathian–Pannonian region [PDF]
This review considers the magmatic processes in the Carpathian–Pannonian Region (CPR) from Early Miocene to Recent times, as well as the contemporaneous magmatism at its southern boundary in the Dinaride and Balkans regions.
Alasonati Tašárová+164 more
core +1 more source
Earth's Continental Lithosphere Through Time
The record of the continental lithosphere is patchy and incomplete; no known rock is older than 4.02 Ga, and less than 5% of the rocks preserved are older than 3 Ga. In addition, there is no recognizable mantle lithosphere from before 3 Ga. We infer that
C. Hawkesworth+3 more
semanticscholar +1 more source
Rifted margins form from extension and breakup of the continentallithosphere. If this extension is coeval with a region of hotter lithosphere,then it is generally assumed that a volcanic margin would follow.
Armitage, J.J.+3 more
core +1 more source
An Evaluation of Proposed Mechanisms of Slab Flattening in Central Mexico [PDF]
Central Mexico is the site of an enigmatic zone of flat subduction. The general geometry of the subducting slab has been known for some time and is characterized by a horizontal zone bounded on either side by two moderately dipping sections.
Clayton, Robert W., Skinner, Steven M.
core +2 more sources
Magmatic record of India-Asia collision [PDF]
This work was financially co-supported by Chinese Academy of Sciences (XDB03010301) and other Chinese funding agencies (Project 973: 2011CB403102 and 2015CB452604; NSFC projects: 41225006, 41273044, and 41472061).New geochronological and geochemical data
Cawood, Peter Anthony+8 more
core +1 more source
Dear Readers, So, do we really need another journal full of papers on solid earth science taking up shelf space in our offices and competing for scarce subscription funds in our libraries? The answer to this question was, in a sense, addressed 150 years ago by Charles Darwin in a somewhat ...
Jon D. Pelletier+2 more
openaire +2 more sources