Results 121 to 130 of about 253 (188)
Mafic slab melt contributions to Proterozoic massif-type anorthosites. [PDF]
Sci AdvKeller DS +6 more
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Litho-structural interpretation of aeromagnetic anomalies reveals potential for mineral exploration in Tizi n'Test Region, Western High Atlas, Morocco. [PDF]
Sci RepDadi B +11 more
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Improved aboveground biomass estimation and regional assessment with aerial lidar in California's subalpine forests. [PDF]
Carbon Balance ManagWinsemius S +5 more
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A biogeographical appraisal of the threatened South East Africa Montane Archipelago ecoregion. [PDF]
Sci RepBayliss J +25 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
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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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Tectonophysics, 1973
Abstract The formation of the melts which produce intrusions of the granite family are considered to result from the partial fusion of high-grade metamorphic rocks. The melting behaviour of such materials is considered. Such melts will rarely be water-saturated and the degree of water-saturation must set limits on the ability of the melt to rise. The
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Abstract The formation of the melts which produce intrusions of the granite family are considered to result from the partial fusion of high-grade metamorphic rocks. The melting behaviour of such materials is considered. Such melts will rarely be water-saturated and the degree of water-saturation must set limits on the ability of the melt to rise. The
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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 ...
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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 ...
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Journal of the Geological Society, 1978
The Mesozoic-Cenozoic Coastal Batholith of Peru is a multiple intrusion of gabbro, tonalite and granite occupying the core of the Western Cordillera over a length of 1600 km. Its structure and composition are described within the context of an intracratonic Andean zone in which vertical movements were dominant.
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The Mesozoic-Cenozoic Coastal Batholith of Peru is a multiple intrusion of gabbro, tonalite and granite occupying the core of the Western Cordillera over a length of 1600 km. Its structure and composition are described within the context of an intracratonic Andean zone in which vertical movements were dominant.
openaire +1 more source