Results 191 to 200 of about 16,733 (259)
Cretaceous coastal mountain building and potential impacts on climate change in East Asia. [PDF]
Li J +7 more
europepmc +1 more source
Surviving a Dark Age: The Oldest Baleen-Bearing Whales (Cetacea: Chaeomysticeti) of Pacific South America (Lower Miocene, Peru). [PDF]
Nobile F +10 more
europepmc +1 more source
Tectonic evolution and mineralization exploration of Lujing uranium ore field, South China. [PDF]
Ren W +8 more
europepmc +1 more source
Re-Os dating of the Makimine and Shimokawa VMS deposits for new age constraints on ridge subduction beneath Japanese Islands. [PDF]
Nozaki T, Takaya Y, Nakayama K, Kato Y.
europepmc +1 more source
Temperature-induced microstructural evolution and fractal characteristics of high-enthalpy Chumathang granite for enhanced geothermal energy. [PDF]
Singh M +8 more
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Science, 1967
The Sierra Nevada batholith is localized in the axial region of a complex faulted synclinorium that coincides with a downfold in the Mohorovicic discontinuity and in P-wave velocity boundaries within the crust. Observed P-wave velocities are compatible with downward increase in the proportion of diorite, quartz diorite, and calcic granodiorite relative
P C, Bateman, J P, Eaton
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The Sierra Nevada batholith is localized in the axial region of a complex faulted synclinorium that coincides with a downfold in the Mohorovicic discontinuity and in P-wave velocity boundaries within the crust. Observed P-wave velocities are compatible with downward increase in the proportion of diorite, quartz diorite, and calcic granodiorite relative
P C, Bateman, J P, Eaton
openaire +2 more sources
Making Space for Batholiths by Extrusion of Sub-Batholithic Crust
International Geology Review, 2003The long-standing space problem in the emplacement of orogenic batholiths may be solved by large-scale intracrustal flow toward the backarc, driven by the isostatic load of the batholith and its volcanic carapace. Isostatic compensation of modern magmatic arcs requires at least the volcanic cover to have settled relative to adjacent rocks.
Allen F. Glazner +3 more
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2021
Wie verschaffen sich Magmen beim Aufstieg den notigen Raum? Die mechanisch einfachste Losung scheint die Aufwolbung der uberlagernden Gesteine zu sein. Am Sandfell in Island ist ein solches Verhalten anschaulich dokumentiert. Das Magma ist hier zwischen Lagen aus Basalt eingedrungen und hat das Dach erkennbar nach oben gewolbt.
openaire +1 more source
Wie verschaffen sich Magmen beim Aufstieg den notigen Raum? Die mechanisch einfachste Losung scheint die Aufwolbung der uberlagernden Gesteine zu sein. Am Sandfell in Island ist ein solches Verhalten anschaulich dokumentiert. Das Magma ist hier zwischen Lagen aus Basalt eingedrungen und hat das Dach erkennbar nach oben gewolbt.
openaire +1 more source
2021
Granit – soweit das Auge blickt. Der Korsisch-Sardische Batholith ist einer der grosten Granitkomplexe Europas. Man trifft darin auf unterschiedlichste Landschaften: Hochflachen, tief eingeschnittene Taler und nur schwer zugangliche Gebirge. Der „Batholith“ – ein Begriff, einst geschaffen fur Granite, die sich in „unendliche Teufe“ erstrecken und ...
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Granit – soweit das Auge blickt. Der Korsisch-Sardische Batholith ist einer der grosten Granitkomplexe Europas. Man trifft darin auf unterschiedlichste Landschaften: Hochflachen, tief eingeschnittene Taler und nur schwer zugangliche Gebirge. Der „Batholith“ – ein Begriff, einst geschaffen fur Granite, die sich in „unendliche Teufe“ erstrecken und ...
openaire +1 more source
Geological Society of America Bulletin, 1931
Conventional Sections and Maps In cross-sections showing granite batholiths, 2 it is customary to depict them as extending down as far as the section goes, bounded by rather steep sides and with no known bottom, which is in accord with the definition of a batholith, but the question may be asked; how far is this due to those limitations of drawing ...
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Conventional Sections and Maps In cross-sections showing granite batholiths, 2 it is customary to depict them as extending down as far as the section goes, bounded by rather steep sides and with no known bottom, which is in accord with the definition of a batholith, but the question may be asked; how far is this due to those limitations of drawing ...
openaire +1 more source

