sequences are also found in the vicinity of the synform: the freshwater Upper Carboniferous sequence is dominated by coarse grained conglomerates and sandstones with subordinate fluvial and lacustrine clays while the Cretaceous sequence is characterised by sandy and clayey lacustrine sediments together with glauconitic sandstones and calcareous siltstones deposited in shallow epicontinental seas.
 provide a detailed description of the N-S striking postorogenic
extensional faults bounding this horst structure and an analysis of the geometry, orientation, and kinematics of all the other tectonic features occurring in the Torre Alfina geothermal system.
(1984), all granitoid samples are clearly found in 'postorogenic
granite' (POG) fields (Fig.
Structural denudation of Silurian-Devonian high-grade metamorphic rocks and postorogenic
detachment faulting in the Maritimes Basin, northern Nova Scotia.
(2011b) date the end of the San Rafael orogeny in relation to the age of intrusion of the postorogenic
Huinganco Granite, i.e.
Agrawal, "Discrimination between late-orogenic, postorogenic
, and anorogenic granites by major element compositions," Journal of Geology, vol.
As the Saaremaa zone crosscuts the post-orogenic plutonic rocks, it can be considered as formed during postorogenic
and anorogenic faulting phases.
Beginning with physical parameters, the list also included important aspects of orogenic and postorogenic
This unit is related to a postorogenic
mantle of carbonate units structured by reverse faults, which have since changed to strike-slip tectonics.
In the context of the Betic Range, Neogene postorogenic
basins provide an important stratigraphic log.
The representatives of postorogenic
magmatism, small monzonite-type mafic-felsic plutons of shoshonitic geochemical affinity, originating from the enriched lithospheric mantle, intruded into southern Finland 1.82-1.77 Ga ago (Eklund et al.
magmatites, mostly A-type granites of Neoproterozoic/early Cambrian age, have been thoroughly studied in continental sectors of the Nubian/Arabian Shield by Harris and Mariner (1980), Radain et al.