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Laurentia's Grenville Loop: Tracking Rodinia Across the Mesoproterozoic to Neoproterozoic Boundary
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- 1 Intro
- 2 The well-dated Keweenawan Track mild post-emplacement thermal histories
- 3 Late Mesoproterozoic Laurentia paleogeography ~25 Myr of rifting and fast plate motion
- 4 No date, No rate
- 5 Previous age interpretation for the Jacobsville Formation
- 6 Field and radiometric constraints on Jacobsville deposition and deformation
- 7 Detrital zircon maximum deposition age constraints using CA-ID-TIMS
- 8 Age constraints on faulting from U-Pb dates on late kinematic fault breccia calcite
- 9 Field and geochronology constraints on Jacobsville deposition and deformation
- 10 Jacobsville paleomagnetism previous work
- 11 Siltstone and fine-grained sandstone beds in the Jacobsville Formation
- 12 Jacobsville paleomagnetism high resolution thermal demagnetization
- 13 Red bed paleomagnetism high-resolution thermal demagnetization
- 14 Positive Intraformational conglomerate test
- 15 Fold test provides age constraints
- 16 Inclination correction using the elongation/inclination method
- 17 Revisiting the Adirondack Highlands thermochronology
- 18 New geochronology data from the Adirondack Highlands
- 19 New thermochronology data from the Adirondack Highlands
- 20 Laurentia at the Center of Rodinia Supercontinent
- 21 Implication for the age of the Grenville Loop
- 22 Revisiting the Grenville poles Brown and McEnroe, 2012
- 23 Laurentia's slowdown after the onset of Grenvillian orogeny
