Ian Hillenbrand
Ian Hillenbrand is a Geologist with the Geosciences and Environmental Change Science Center
Science and Products
Filter Total Items: 15
Geochemical evidence for evolving Proterozoic crustal thickness and orogenic styles in southwestern Laurentia Geochemical evidence for evolving Proterozoic crustal thickness and orogenic styles in southwestern Laurentia
It has long been challenging for researchers to track the crustal thickness and mode(s) of crustal modification in ancient convergent margins, limiting evaluation of the tectonic styles and processes that modify continental crust during orogenesis. We present trace element igneous geochemical crustal thickness proxies that quantitatively track the crustal thickness evolution of the long...
Authors
Ian Hillenbrand, Karl Karlstrom, Michael Williams, Amy Gilmer, Wayne Premo, Peter Davis
Monazite and xenotime petrochronologic constraints on four Proterozoic tectonic episodes and ca. 1705 Ma age of the Uncompahgre Formation, southwestern Colorado, USA Monazite and xenotime petrochronologic constraints on four Proterozoic tectonic episodes and ca. 1705 Ma age of the Uncompahgre Formation, southwestern Colorado, USA
The Proterozoic tectonic evolution of the south-western USA remains incompletely understood due to limited constraints on the timing and conditions of the tectono-metamorphic phases and depositional age of metasedimentary successions. We integrated multi-scale compositional mapping, petrologic modeling, and in situ geochronology to constrain pressure-temperature-time paths from samples...
Authors
Ian Hillenbrand, Michael Williams, Karl Karlstrom, Amy Gilmer, Heather Lowers, Michael Jercinovic, Kaitlyn Suarez, Amanda Souders
Geochemical evidence for diachronous uplift and synchronous collapse of the high elevation Variscan hinterland Geochemical evidence for diachronous uplift and synchronous collapse of the high elevation Variscan hinterland
Competing end-member models for the late Paleozoic Variscan orogeny (ca. 360-290 Ma) alternatively suggest moderate 2-3 km elevations underlain by relatively thin crust (55 km) that supported high 4-5 km elevations. We tested these models and quantified the crustal thickness and elevation evolution of the Variscan orogeny using igneous trace element geochemical proxies. The data suggest...
Authors
Ian Hillenbrand, Michael Williams
Science and Products
Filter Total Items: 15
Geochemical evidence for evolving Proterozoic crustal thickness and orogenic styles in southwestern Laurentia Geochemical evidence for evolving Proterozoic crustal thickness and orogenic styles in southwestern Laurentia
It has long been challenging for researchers to track the crustal thickness and mode(s) of crustal modification in ancient convergent margins, limiting evaluation of the tectonic styles and processes that modify continental crust during orogenesis. We present trace element igneous geochemical crustal thickness proxies that quantitatively track the crustal thickness evolution of the long...
Authors
Ian Hillenbrand, Karl Karlstrom, Michael Williams, Amy Gilmer, Wayne Premo, Peter Davis
Monazite and xenotime petrochronologic constraints on four Proterozoic tectonic episodes and ca. 1705 Ma age of the Uncompahgre Formation, southwestern Colorado, USA Monazite and xenotime petrochronologic constraints on four Proterozoic tectonic episodes and ca. 1705 Ma age of the Uncompahgre Formation, southwestern Colorado, USA
The Proterozoic tectonic evolution of the south-western USA remains incompletely understood due to limited constraints on the timing and conditions of the tectono-metamorphic phases and depositional age of metasedimentary successions. We integrated multi-scale compositional mapping, petrologic modeling, and in situ geochronology to constrain pressure-temperature-time paths from samples...
Authors
Ian Hillenbrand, Michael Williams, Karl Karlstrom, Amy Gilmer, Heather Lowers, Michael Jercinovic, Kaitlyn Suarez, Amanda Souders
Geochemical evidence for diachronous uplift and synchronous collapse of the high elevation Variscan hinterland Geochemical evidence for diachronous uplift and synchronous collapse of the high elevation Variscan hinterland
Competing end-member models for the late Paleozoic Variscan orogeny (ca. 360-290 Ma) alternatively suggest moderate 2-3 km elevations underlain by relatively thin crust (55 km) that supported high 4-5 km elevations. We tested these models and quantified the crustal thickness and elevation evolution of the Variscan orogeny using igneous trace element geochemical proxies. The data suggest...
Authors
Ian Hillenbrand, Michael Williams