The late exhumation history of the ultrahigh-pressure Maksyutov Complex, south Ural Mountains, from new apatite fission track data

Tectonics ◽  
2000 ◽  
Vol 19 (1) ◽  
pp. 153-167 ◽  
Author(s):  
Mary L. Leech ◽  
Daniel F. Stockli
Keyword(s):  
Fission Track ◽  
Ultrahigh Pressure ◽  
Apatite Fission Track ◽  
Ural Mountains ◽  
Maksyutov Complex ◽  
History Of ◽  
Exhumation History

Long-term exhumation history of the Inner Mongolian Plateau constrained by apatite fission track analysis

2016 ◽  
Vol 666 ◽  
pp. 121-133 ◽  
Author(s):  
Ke Li ◽  
Marc Jolivet ◽  
Zhicheng Zhang ◽  
Jianfeng Li ◽  
Wenhao Tang
Keyword(s):  
Fission Track ◽  
Apatite Fission Track ◽  
Mongolian Plateau ◽  
Fission Track Analysis ◽  
History Of ◽  
Track Analysis ◽  
Exhumation History

scholarly journals Thermochronology and Exhumation History of the Northeastern Fennoscandian Shield Since 1.9 Ga: Evidence From 40 Ar/ 39 Ar and Apatite Fission Track Data From the Kola Peninsula

Tectonics ◽  
2019 ◽  
Vol 38 (7) ◽  
pp. 2317-2337 ◽  
Author(s):  
Roman V. Veselovskiy ◽  
Stuart N. Thomson ◽  
Andrey A. Arzamastsev ◽  
Svetlana Botsyun ◽  
Aleksey V. Travin ◽  
...  
Keyword(s):  
Kola Peninsula ◽  
Fission Track ◽  
Fennoscandian Shield ◽  
Apatite Fission Track ◽  
History Of ◽  
Exhumation History

scholarly journals New insights into the Gondwana breakup at the Southern South America by apatite fission-track analyses

2019 ◽  
Vol 47 ◽  
pp. 1-15 ◽  
Author(s):  
Cristiane H. Gomes ◽  
Delia Almeida
Keyword(s):  
Fission Track ◽  
Shear Zones ◽  
Temperature History ◽  
Early Paleozoic ◽  
Apatite Fission Track ◽  
Pan African ◽  
History Of ◽  
Dom Feliciano Belt ◽  
Eastern Domain ◽  
Exhumation History

Abstract. Apatite fission-track (AFT) analyses, applied to Southern Brazil and Uruguay samples, was employed aiming to understand the low temperature history of the Dom Feliciano Belt Segment. The Dom Feliciano Belt formed during the Neoproterozoic to Early Paleozoic, linked to the Brasiliano/Pan-African Orogeny. Twenty-four samples were dated, and confined track lengths of twenty samples were measured. The spatial distribution of ages shows three domains with different evolution cut by shear zones and, or suture zones in the Dom Feliciano Belt. The Western Domain exhibits AFT ages > 250 Ma (Permian to Devonian) while the Eastern Domain shows AFT ages < 230 Ma (Paleogene to Triassic). In the Central Domain, the AFT ages range from ∼196 to 130 Ma (Jurassic to Early Cretaceous). The thermal modeling in the domains revealed a complex evolution, with cooling and reheating phases, and a denudation of ∼2600 m. The AFT ages clearly postdate the Gondwanide, Paraná-Etendeka and Rio Grande Cone exhumation history of the Dom Feliciano Belt.

Low-temperature exhumation history of Variscan-age rocks in the western Cantabrian Mountains (NW Spain) recorded by apatite fission-track data

2010 ◽  
Vol 489 (1-4) ◽  
pp. 76-90 ◽  
Author(s):  
René W. Grobe ◽  
Joaquina Alvarez-Marrón ◽  
Ulrich A. Glasmacher ◽  
Rosana Menéndez-Duarte
Keyword(s):  
Low Temperature ◽  
Fission Track ◽  
Apatite Fission Track ◽  
Cantabrian Mountains ◽  
Nw Spain ◽  
History Of ◽  
Exhumation History
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