Results 241 to 250 of about 36,045 (295)

Late Quaternary activities of the Xinbaoan-Shacheng fault in the North China Plain. [PDF]

Sci Rep
Qiu C, Yu Z, Li L, Wang W, Zhao Q, Zheng R, Yang Y.   +6 more
europepmc   +1 more source

High-enthalpy Larderello geothermal system, Italy, powered by thousands of cubic kilometres of mid-crustal magma. [PDF]

Commun Earth Environ
Lupi M, Stumpp D, Cabrera-Pérez I, Michailos K, Saccorotti G, Bonini M, Farina F, Jiwani-Brown EA, Lanari R, Papeschi S, Savard G, Porras J, Sfalcin J, Muñoz-Burbano F, Minetto R, Del Ventisette C, Piccinini D, Montanari D.   +17 more
europepmc   +1 more source

Mantle-derived fluid flux controls Olympic Dam-style Fe oxide-Cu-Au mineralisation. [PDF]

Sci Rep
Thiel S, Reid A, Heinson G, Brand K, Li L.   +4 more
europepmc   +1 more source

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Cenozoic tectonic inversion in the Naglfar Dome, Norwegian North Sea

Marine and Petroleum Geology, 2020
Abstract Extensional settings with multiple phases of rifting are often intermitted by compressional tectonics or inversion. Differentiating compressional structures/phases in such settings become difficult when magma-induced forced folds are also present.
K O Omosanya
exaly   +2 more sources

Inversion tectonics in central Alborz, Iran

Journal of Structural Geology, 2006
Abstract Structural analyses carried out in the southern-central Alborz (Iran) have shown that the evolution of this belt has been strongly conditioned by the inversion of pre-existent extensional faults. Inversion tectonics has been identified especially in the southern part of the belt, and it is related to the reactivation of grabens formed in the
ZANCHI, ANDREA MARCO, Berra, F, Mattei, M, Ghassemi, M, Sabouri, J.   +4 more
openaire   +3 more sources

Geometry and kinematics of inversion tectonics

Geological Society, London, Special Publications, 1989
Summary Positive inversion tectonics involves the reversal of extensional fault movement during contractional tectonics. Basin stratigraphy developed before, during and after extensional fault movements may be described as pre-, syn- and postrift sequences.
G. D. Williams, C. M. Powell, M. A. Cooper   +2 more
openaire   +1 more source

Sandbox model studies of inversion tectonics

Tectonophysics, 1987
Abstract Scaled plane-strain sandbox models have been used to simulate basement-controlled structural inversion in a sedimentary overburden. Two basement configurations were tested. In the first one, reversal of movement along vertical and normal faults that controlled a graben relief induced only a partial recovery of displacement along the pre ...
A. Koopman, A. Speksnijder, W.T. Horsfield   +2 more
openaire   +1 more source

Mid-continent tectonic inversions, Northwest Territories, Canada

Journal of Structural Geology, 1996
Abstract Four types of tectonic inversion are recorded on reflection seismic data from the area northwest of Great Bear Lake in the Northwest Territories, Canada. The strata involved span about 1.7 Ga of Proterozoic and Phanerozoic history, and have been subjected to at least five tectonic events, two extensional, two compressional and one ...
D.G. Cook, B.C. MacLean
openaire   +1 more source

Analogue models of inversion tectonics

Geological Society, London, Special Publications, 1989
Summary Inversion of dip-slip fault systems by horizontal recompression has been modelled using sand, sand-mica and sand-clay analogues. Three extension-inversion systems have been tested: uniform basal detachment, simple listric detachment and ramp/flat detachments.
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Inversion tectonics in S.W. Dyfed

Proceedings of the Geologists' Association, 1987
Inverted sedimentary basins form when basin-controlling extensional faults reverse their movement during contractional tectonics. The structural evolution of S.W. Dyfed is considered in terms of a model of positive inversion tectonics. A change in deformation mode from Devonian extension to Late Carboniferous contraction gave rise to renewed movement ...
openaire   +1 more source