Results 111 to 120 of about 5,395 (224)

The role of extension in the Miocene denudation of the Nevado-Filábride Complex, Betic Cordillera (SE Spain) [PDF]

, 2004
The Internal Zone of the Betic Cordillera, SE Spain, consists of a nappe stack of three complexes, the deepest of which is the Nevado-Filábride Complex.
Harbury, N, Hurford, AJ, Johnson, C
core   +1 more source

Bayesian Markov-Chain Monte Carlo Inversion of Low-Temperature Thermochronology Around Two 8 − 10 m Wide Columbia River Flood Basalt Dikes

Frontiers in Earth Science, 2019
Flood basalt volcanism involves large volumes of magma emplaced into the crust and surface environment on geologically short timescales. The mechanics of flood basalt emplacement, including dynamics of the crustal magma transport system and the tempo of ...
Leif Karlstrom, Kendra E. Murray, Peter W. Reiners   +2 more
doaj   +1 more source

Low-temperature thermochronometry along the Kunlun and Haiyuan Faults, NE Tibetan Plateau: Evidence for kinematic change during late-stage orogenesis [PDF]

, 2013
The Tibetan Plateau is a prime example of a collisional orogen with widespread strike-slip faults whose age and tectonic significance remain controversial.
Clark, Marin K., Craddock, William H., Duvall, Alison R., Farley, Kenneth A., Kirby, Eric, Li, Chuanyou, Yuan, Dao-Yang   +6 more
core   +3 more sources

Multianalytical provenance analysis of Eastern Ross Sea LGM till sediments (Antarctica): Petrography, geochronology, and thermochronology detrital data [PDF]

, 2017
In order to reveal provenance of detrital sediments supplied by West Antarctic Ice Sheet (WAIS), 19 glaciomarine cores of Last Glacial Maximum age were analyzed from Eastern Ross Sea and Sulzberger Bay.
Andreucci, Benedetta, Langone, Antonio, Perotti, Matteo, Talarico, Franco, Zattin, Massimiliano   +4 more
core   +2 more sources

Widespread late Cenozoic increase in erosion rates across the interior of eastern Tibet constrained by detrital low-temperature thermochronometry [PDF]

, 2012
New detrital low-temperature thermochronometry provides estimates of long-term erosion rates and the timing of initiation of river incision from across the interior of the Tibetan Plateau.
Avdeev, Boris, Chen, Zhengwei, Clark, Marin K., Duvall, Alison R., Farley, Kenneth A.   +4 more
core   +2 more sources

The Thermal Evolution of Western Norway Based on Multi‐Sample Models of an Elevation Transect: Implications for the Formation of High‐Elevation Low‐Relief Surfaces on an Elevated Rifted Continental Margin

Geochemistry, Geophysics, Geosystems
The post‐Caledonian thermal and geomorphological evolution of onshore Western Norway is poorly understood, including the formation and age of the high‐elevation low‐relief surfaces seen across the Norwegian landscape. We present new apatite fission track
Å. Hestnes, D. Gasser, R. Ketcham, I. Dunkl, A. K. Ksienzyk, T. Scheiber, H. Sirevaag, J. Jacobs   +7 more
doaj   +1 more source

Thermal evolution of Cathaysian block along the South China margin since the Late Cretaceous: evidence from low-temperature thermochronology

Frontiers in Earth Science
The Cathaysian Block has undergone complex tectonic transformation since the Mesozoic, with significant topographic and geomorphological changes due to large-scale magmatism, as well as tectonism in the central area.
Hongcai Shi, Hongcai Shi, Hui Xie, Hui Xie, Hui Xie, Weina Zhao, Tangwei Liu, Deming Kong, Deming Kong, Chuang Bao, Chuang Bao, Lijie Liu   +11 more
doaj   +1 more source

Upper Cretaceous exhumation of the western Rhodope Metamorphic Province (Chalkidiki Peninsula, northern Greece)

, 2014
International audienceThe Vertiskos Unit of northern Greece is an elongated basement belt with a complex poly-metamorphic history. It extends from Greece (Chalkidiki peninsula), to the south, up to Serbia, in the north, and arguably represents the ...
Brun, Jean-Pierre, Gallagher, Kerry, Gueydan, Frédéric, Jolivet, Marc, Kostopoulos, Dimitrios, Kydonakis, Konstantinos   +5 more
core   +4 more sources

Ultra-low-temperature Thermochronology Using Optically Stimulated Luminescence (OSL)

RADIOISOTOPES, 2021
Manabu Ogata, Shigeru Sueoka
openaire   +2 more sources

The Gulf of Suez rifting: implications from low-temperature thermochronology

International Geology Review
The Gulf of Suez is a continental rift basin that has been developed during the Oligocene-Miocene as a northern extension of the Red Sea rift system. The Oligo-Miocene rift-activated flanks are represented by exposures of the Neoproterozoic basement rocks of the Arabian-Nubian Shield. An additional thermal overprint (i.e.
Mansour, Sherif, Hasebe, Noriko, Abdelrahman, Kamal, Fnais, Mohammed S., Tamura, Akihiro   +4 more
openaire   +1 more source