Evidence of displacement-driven maturation along the San Cristobal Trough transform plate boundary

2018 ◽  
Vol 485 ◽  
pp. 88-98 ◽  
Author(s):  
James S. Neely ◽  
Kevin P. Furlong
Keyword(s):  
Plate Boundary ◽  
Transform Plate Boundary

scholarly journals Fault slip beyond a barrier on a transform plate boundary

1983 ◽  
Vol 75 (1) ◽  
pp. 143-153 ◽  
Author(s):  
M. Bonafede ◽  
E. Boschi ◽  
M. Dragoni
Keyword(s):  
Plate Boundary ◽  
Fault Slip ◽  
Transform Plate Boundary

Morphostructure of an incipient subduction zone along a transform plate boundary: Puysegur Ridge and Trench

Geology ◽  
1995 ◽  
Vol 23 (6) ◽  
pp. 519 ◽  
Author(s):  
Jean-Yves Collot ◽  
Geoffroy Lamarche ◽  
Ray A. Wood ◽  
Jean Delteil ◽  
Marc Sosson ◽  
...  
Keyword(s):  
Subduction Zone ◽  
Plate Boundary ◽  
Transform Plate Boundary

scholarly journals Extension along the Australian-Pacific transpressional transform plate boundary near Macquarie Island

2003 ◽  
Vol 4 (9) ◽  
pp. n/a-n/a ◽  
Author(s):  
Nathan R. Daczko ◽  
Karah L. Wertz ◽  
Sharon Mosher ◽  
Millard F. Coffin ◽  
Tip A. Meckel
Keyword(s):  
Plate Boundary ◽  
Macquarie Island ◽  
Transform Plate Boundary

scholarly journals Deformation between the highly oblique Yakutat–North American plate boundary and the Eastern Denali fault

Geosphere ◽  
2021 ◽  
Author(s):  
Eva Enkelmann ◽  
Sarah Falkowski
Keyword(s):  
North American ◽  
Temporal Pattern ◽  
Fission Track ◽  
Plate Boundary ◽  
North American Plate ◽  
Late Cenozoic ◽  
Denali Fault ◽  
Zircon Fission Track ◽  
Transform Plate Boundary ◽  
River Catchments

This study investigates the spatial and temporal pattern of rock exhumation inboard of the highly oblique Yakutat–North American plate boundary. We aim to quantify how far deformation is transferred inboard of the Fairweather transform plate boundary and across the Eastern Denali fault. We present new detrital apatite and zircon fission track data from 27 modern drainages collected on both sides of the Eastern Denali fault and from the Alsek and Tatshenshini River catchments that drain the mountainous region between the Fairweather fault and the Eastern Denali fault. By integrating our data with published bedrock and detrital geochronology and thermochronology, we show that exhumation reaches much farther inboard (>100 km) of the Fairweather fault than farther north in the St. Elias syntaxial region (<30 km). This suggests that the entire corridor between the Fairweather and Eastern Denali faults exhumed since mid-Miocene time. The Eastern Denali fault appears to be the backstop, and late Cenozoic exhumation northeast of the fault is very limited.

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