The North American Cordillera influences climate on a local and global scale, by forming a distinct barrier to Pacific moisture reaching the continental interior. The extent to which this climatic pattern existed in the past is uncertain, so improving our understanding of the elevation history of the Cordillera is critical to determining the controls on climate change within the Northern Hemisphere [e.g. Foster et al. 2010]. In western Canada, the Cordillera comprises two parallel mountain chains separated by a high elevation (~1100 m) intermontane plateau. The Cenozoic exhumation history of the western range, the Coast Mountains, has been well studied [e.g. Parrish, 1983; O'Sullivan and Parrish, 1995; Farley et al., 2001], while the Cenozo...
Apatite (U-Th)/He ages reveal three distinct periods in the exhumation history of the northern Coast...
A detailed structural and metamorphic study along a transect from the core of the Thor-Odin dome to ...
The Central Andes between 18°S and 36°S latitude strike north-south for 2000 km along the Chilean su...
The North American Cordillera influences climate on a local and global scale, by forming a distinct ...
International audienceNew low temperature thermochronology data from clastic sedimentary rocks in th...
Fission track dating of zircon and apatite has been used to determine the Cenozoic uplift history of...
No consensus exists on the mechanisms that caused surface uplift and high elevations in the southern...
Aim Although ongoing climate change is expected to lead to an upward shift of tree lines in mountai...
Nearly all of what is now British Columbia and adjacent areas were covered by an ice sheet at the ma...
The Thor-Odin dome is a basement-cored tectonothermal culmination in southern British Columbia conta...
Continental topography is the result of complex interactions among mantle convection, continental dy...
Resolving the linkages among climate, erosion, and tectonics has implications for understanding geol...
Apatite (U-Th)/He ages reveal three distinct periods in the exhumation history of the central Coast ...
International audienceAbstract During the last glacial maximum the Cordilleran and Laurentide ice sh...
We present new multiscale structural, mineral chemical, and U-Pb isotope dilution\u2013thermal ioniz...
Apatite (U-Th)/He ages reveal three distinct periods in the exhumation history of the northern Coast...
A detailed structural and metamorphic study along a transect from the core of the Thor-Odin dome to ...
The Central Andes between 18°S and 36°S latitude strike north-south for 2000 km along the Chilean su...
The North American Cordillera influences climate on a local and global scale, by forming a distinct ...
International audienceNew low temperature thermochronology data from clastic sedimentary rocks in th...
Fission track dating of zircon and apatite has been used to determine the Cenozoic uplift history of...
No consensus exists on the mechanisms that caused surface uplift and high elevations in the southern...
Aim Although ongoing climate change is expected to lead to an upward shift of tree lines in mountai...
Nearly all of what is now British Columbia and adjacent areas were covered by an ice sheet at the ma...
The Thor-Odin dome is a basement-cored tectonothermal culmination in southern British Columbia conta...
Continental topography is the result of complex interactions among mantle convection, continental dy...
Resolving the linkages among climate, erosion, and tectonics has implications for understanding geol...
Apatite (U-Th)/He ages reveal three distinct periods in the exhumation history of the central Coast ...
International audienceAbstract During the last glacial maximum the Cordilleran and Laurentide ice sh...
We present new multiscale structural, mineral chemical, and U-Pb isotope dilution\u2013thermal ioniz...
Apatite (U-Th)/He ages reveal three distinct periods in the exhumation history of the northern Coast...
A detailed structural and metamorphic study along a transect from the core of the Thor-Odin dome to ...
The Central Andes between 18°S and 36°S latitude strike north-south for 2000 km along the Chilean su...