Results 241 to 250 of about 692,725 (319)
Some of the next articles are maybe not open access.
Tectonics, 2022
The orogenic growth of the Domeyko Cordillera was induced by a positive tectonic inversion. In this work, we have validated this interpretation from new field data, which were combined with 2‐D reflection seismic profile interpretations obtained along ...
C. López +10 more
semanticscholar +1 more source
The orogenic growth of the Domeyko Cordillera was induced by a positive tectonic inversion. In this work, we have validated this interpretation from new field data, which were combined with 2‐D reflection seismic profile interpretations obtained along ...
C. López +10 more
semanticscholar +1 more source
, 2021
The Permian to early Triassic terrestrial successions in the Mahu sag constrain the tectonic evolution of northwestern edge of the Junggar basin. This study analyzes the sequence stratigraphy of the Mahu sag in order to understand the interplay between ...
Wenbin Tang +5 more
semanticscholar +1 more source
The Permian to early Triassic terrestrial successions in the Mahu sag constrain the tectonic evolution of northwestern edge of the Junggar basin. This study analyzes the sequence stratigraphy of the Mahu sag in order to understand the interplay between ...
Wenbin Tang +5 more
semanticscholar +1 more source
, 2021
The Northern Depression of the South Yellow Sea Basin underwent two episodes of tectonic inversion from the latest Eocene to Oligocene and in the Pliocene, respectively. During the inversion, the structural depression controlled previously by extensional
Ruoyu Zhang +4 more
semanticscholar +1 more source
The Northern Depression of the South Yellow Sea Basin underwent two episodes of tectonic inversion from the latest Eocene to Oligocene and in the Pliocene, respectively. During the inversion, the structural depression controlled previously by extensional
Ruoyu Zhang +4 more
semanticscholar +1 more source
CENOZOIC TECTONIC INVERSION IN THE BANDAR JISSAH AREA, OMAN
Geological Society of America Abstracts with ProgramsEran Driscoll, Christopher M. Bailey
openaire +2 more sources
Basin Research, 2020
Common basin models assume that the post‐rift tectonic evolution of most basins is usually associated with tectonic quiescence. However, tectonic inversion during the post‐rift phase has been proposed for several sedimentary basins worldwide, but how and
D. L. Vasconcelos +6 more
semanticscholar +1 more source
Common basin models assume that the post‐rift tectonic evolution of most basins is usually associated with tectonic quiescence. However, tectonic inversion during the post‐rift phase has been proposed for several sedimentary basins worldwide, but how and
D. L. Vasconcelos +6 more
semanticscholar +1 more source
Inversion tectonics in central Alborz, Iran
Journal of Structural Geology, 2006Abstract 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 +4 more
openaire +3 more sources
, 2020
The tectonic inversion of the Songliao Basin during the Oligo–Miocene may have played an important role in controlling the development of sandstone-type uranium deposits (SUDs).
Yinhang Cheng +6 more
semanticscholar +1 more source
The tectonic inversion of the Songliao Basin during the Oligo–Miocene may have played an important role in controlling the development of sandstone-type uranium deposits (SUDs).
Yinhang Cheng +6 more
semanticscholar +1 more source
, 2020
The marginal fault system, which is represented by the Hong–Che (Hongshanzui–Chepaizi), Ke–Bai (Karamay–Baikouquan), and Wu–Xia (Wuerhe–Xiazijie) sub-systems and developed in the northwestern margin of the Junggar Basin, NW China, is a key factor ...
Yuanyuan Liang +4 more
semanticscholar +1 more source
The marginal fault system, which is represented by the Hong–Che (Hongshanzui–Chepaizi), Ke–Bai (Karamay–Baikouquan), and Wu–Xia (Wuerhe–Xiazijie) sub-systems and developed in the northwestern margin of the Junggar Basin, NW China, is a key factor ...
Yuanyuan Liang +4 more
semanticscholar +1 more source
Geometry and kinematics of inversion tectonics
Geological Society, London, Special Publications, 1989Summary 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 +2 more
openaire +1 more source
Sandbox model studies of inversion tectonics
Tectonophysics, 1987Abstract 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 +2 more
openaire +1 more source

