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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
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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.
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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.
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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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