Results 151 to 160 of about 21,455 (215)

Diversities of chromite mineralization induced by chemo-thermal evolution of the mantle during subduction initiation. [PDF]

Nat Commun
Zhang PF, Zhou MF, Robinson PT, Malpas J, Yumul GP, Wang CY, Li J.   +6 more
europepmc   +1 more source

Tectonic and climatic implications of the Aleutian Arc initiation ≥56 million years ago. [PDF]

Nat Commun
Hoernle K, Jicha B, Portnyagin M, Zahirovic S, Müller D, Hauff F, Timm C, Höfig TW, Yogodzinski G, Guillong M, Berndt C, Savelyev D, Bezard R, Baranov B.   +13 more
europepmc   +1 more source

Distinct patterns of volcano deformation for hot and cold magmatic systems. [PDF]

Nat Commun
Weber G, Biggs J, Annen C.
europepmc   +1 more source

Uplift of the Tibetan Plateau driven by mantle delamination from the overriding plate. [PDF]

Nat Geosci
Xie Y, Balázs A, Gerya T, Xiong X.
europepmc   +1 more source

Author Correction: Mobility of South America's transcontinental drainage divide and shrinkage of the Paraná river basin linked to lithologic and geodynamic controls. [PDF]

Sci Rep
Crelier C, Zumba A, Peifer D, Val P.
europepmc   +1 more source

Probing the world's largest oceanic plateau: from making to collision. [PDF]

Natl Sci Rev
Jiang X, Li ZX, Gong W, Xing L, Li D, Liu H, Xu C.   +6 more
europepmc   +1 more source

Magmatism in Eastern Paraguay: occurrence and petrography.

, 1995
CENSI P, GOMES C. B, DE MIN, ANGELO, CUNDARI A, VELAZQUEZ V. F., COMIN CHIARAMONTI P   +5 more
core  

Early Miocene magmatism in the Baiyun Sag (South China Sea): A view to the origin of intense post-rift magmatism [PDF]

Gondwana Research, 2023
Post-rift magmatism associated with seafloor spreading (∼32 Ma to ∼15 Ma) and post-spreading tectonics (from ∼15 Ma to the present day) is widely recorded in the South China Sea (SCS).
Qiliang Sun, Tiago M Alves, Shiguo Wu
exaly   +2 more sources

Geochemistry and tectonic development of Cenozoic magmatism in the Carpathian–Pannonian region [PDF]

Gondwana Research, 2011
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.
Ioan Seghedi, Hilary Downes
exaly   +2 more sources

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Magmatic Epidote

Reviews in Mineralogy and Geochemistry, 2004
Epidote was first recognized as a magmatic mineral in the alpine Bergell tonalite by Cornelius (1915). Field observations and microscopic textures let Cornelius to conclude "... the only possibility is, that epidote is a primary mineral in our tonalite, crystallizing early from the magma, i.e., before (in part also contemporaneous with) biotite ...
M. W. Schmidt, S. Poli
openaire   +5 more sources