Resolving the history of early fault slip and foreland basin evolution along the Wyoming salient of the Sevier fold-and-thrust belt: Integrating detrital zircon geochronology, provenance modeling, and subsidence analysis

2018 ◽  
Author(s):  
A. Gentry ◽  
W.A. Yonkee ◽  
M.L. Wells ◽  
E.A. Balgord
Keyword(s):  
Detrital Zircon ◽  
Foreland Basin ◽  
Fault Slip ◽  
Basin Evolution ◽  
Zircon Geochronology ◽  
Thrust Belt ◽  
Detrital Zircon Geochronology ◽  
Fold And Thrust Belt ◽  
Subsidence Analysis ◽  
History Of

scholarly journals Application of Foreland Basin Detrital‐Zircon Geochronology to the Reconstruction of the Southern and Central Appalachian Orogen

2010 ◽  
Vol 118 (1) ◽  
pp. 23-44 ◽  
Author(s):  
Hyunmee Park ◽  
David L. Barbeau Jr. ◽  
Alan Rickenbaker ◽  
Denise Bachmann‐Krug ◽  
George Gehrels
Keyword(s):  
Detrital Zircon ◽  
Foreland Basin ◽  
Zircon Geochronology ◽  
Detrital Zircon Geochronology ◽  
Appalachian Orogen

scholarly journals Sandstone Petrology and Provenance in Fold Thrust Belt and Foreland Basin System

2021 ◽  
Author(s):  
Salvatore Critelli ◽  
Sara Criniti
Keyword(s):  
Foreland Basin ◽  
Thrust Belt ◽  
Fold And Thrust Belt ◽  
Continental Block ◽  
Wide Range ◽  
Geodynamic Processes ◽  
Dual Plate ◽  
History Of ◽  
Sandstone Composition ◽  
Main Producer

The sandstone composition of foreland basin has a wide range of provenance signatures, reflecting the interplay between flexed underplate region and abrupt growth of the accreted upper plate region. The combination of contrasting detrital signatures reflects these dual plate interactions; indeed, several cases figure out that the earliest history of older foreland basin infilling is marked by quartz-rich sandstones, with cratonal or continental-block provenance of the flexed underplate flanks. As upper plate margin grows over the underplate, the nascent fold-and-thrust belt starts to be the main producer of grain particles, reflecting the space/time dependent progressive unroofing of the subjacent orogenic source terranes. The latter geodynamic processes are mainly reflected in the nature of sandstone compositions that become more lithic fragment-rich and feldspar-rich as the fold-thrust belt involves the progressive deepest portions of upper plate crustal terranes. In this context sandstone signatures reflect quartzolithic to quartzofeldspathic compositions.

Detrital-zircon geochronology of the eastern Magallanes foreland basin: Implications for Eocene kinematics of the northern Scotia Arc and Drake Passage

2009 ◽  
Vol 284 (3-4) ◽  
pp. 489-503 ◽  
Author(s):  
David L. Barbeau ◽  
Eduardo B. Olivero ◽  
Nicholas L. Swanson-Hysell ◽  
Khandaker M. Zahid ◽  
Kendra E. Murray ◽  
...  
Keyword(s):  
Detrital Zircon ◽  
Foreland Basin ◽  
Drake Passage ◽  
Zircon Geochronology ◽  
Detrital Zircon Geochronology ◽  
Scotia Arc

Multi-dimensional scaling of detrital zircon geochronology constrains basin evolution of the late Mesoproterozoic Paranoá Group, central Brazil

2021 ◽  
Vol 365 ◽  
pp. 106381
Author(s):  
Marina Seraine ◽  
José Eloi Guimarães Campos ◽  
Marco Antonio Caçador Martins-Ferreira ◽  
Carlos José Souza de Alvarenga ◽  
Farid Chemale ◽  
...  
Keyword(s):  
Detrital Zircon ◽  
Basin Evolution ◽  
Zircon Geochronology ◽  
Detrital Zircon Geochronology ◽  
Central Brazil ◽  
Dimensional Scaling ◽  
Multi Dimensional Scaling
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