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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Antarctica
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Victoria Land
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McMurdo dry valleys (1)
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Chalk Aquifer (1)
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Green Mountains (1)
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North America (1)
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United States
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New England (1)
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commodities
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brines (1)
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metal ores
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uranium ores (1)
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geologic age
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Cenozoic
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Tertiary
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Paleogene
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Oligocene
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Fontainebleau Sandstone (1)
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Paleozoic (1)
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igneous rocks
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igneous rocks
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plutonic rocks
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diabase (1)
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minerals
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carbonates (1)
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sulfates
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gypsum (1)
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Primary terms
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Antarctica
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Victoria Land
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McMurdo dry valleys (1)
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brines (1)
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Cenozoic
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Tertiary
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Paleogene
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Oligocene
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Fontainebleau Sandstone (1)
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crust (1)
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data processing (1)
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faults (1)
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ground water (2)
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heat flow (1)
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igneous rocks
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plutonic rocks
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diabase (1)
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intrusions (1)
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magmas (1)
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mantle (1)
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metal ores
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uranium ores (1)
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metamorphism (1)
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North America (1)
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orogeny (1)
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Paleozoic (1)
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plate tectonics (1)
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sedimentary rocks
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carbonate rocks
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chalk (1)
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limestone
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micrite (1)
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clastic rocks
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sandstone (1)
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structural geology (1)
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tectonics (1)
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United States
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New England (1)
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sedimentary rocks
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sedimentary rocks
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carbonate rocks
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chalk (1)
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limestone
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micrite (1)
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clastic rocks
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sandstone (1)
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Peclet number
Reactive Transport in Evolving Porous Media
Lattice Boltzmann Modeling of Classic Solute Transport Boundary Value Problems
Implications of pore microgeometry heterogeneity for the movement and chemical reactivity of CO 2 in carbonates
Pore Scale Processes Associated with Subsurface CO 2 Injection and Sequestration
Cratonic basins and the long-term subsidence history of continental interiors
A parameter sensitivity analysis of two Chalk tracer tests
Which effective viscosity?
Heat transfer and fault geometry in the Taconian thrust belt, western New England
Tectonic models of the Taconian orogeny in western New England must account for the rapid metamorphism of the Taconic klippen after thrusting. The most likely source of heat for this metamorphism is an overlying hot thrust sheet of accretionary wedge material, which overrode the continental margin of ancient North America, culminating in a continent-island arc collision. Thermal calculations indicate that rapid conductive heat transfer from such a sheet is possible. The dimensionless Peclet number suggests that conductive heat transfer is faster than, or operates at rates comparable to, advective heat transfer due to thrusting over a distance of at least 6 km from a thrust surface. Thus, syntectonic heating of footwall rocks below a major thrust surface is important and must be taken into account in tectonic models. The continental margin thrust system (CMTS) in western New England may have formed as a set of duplexes under a main roof thrust separating the CMTS from the overriding thrust sheet of accretionary wedge material and above a main floor thrust along which the CMTS was transported over autochthonous continental margin rocks. Thrust sheets in this system are composed of Middle Proterozoic Grenville basement and/or upper Proterozoic to Middle Ordovician cover rocks of a western shelf sequence or eastern slope-rise sequence. According to this duplex model, thrust faults tended to develop sequentially toward the foreland, in the transport direction. The relative timing of thrusting and metamorphism is an important constraint on tectonic models, but metamorphism is not a reliable datum with which to compare the timing of events in different parts of the thrust belt. As an example, synmetamorphic thrusting in the eastern internal part of the belt may have preceded brittle faulting to the west near the foreland. P-T paths of rocks from different thrust sheets separated by major faults will be qualitatively different, and detailed petrologic studies to determine and compare P-T paths from different thrust sheets may be useful in identifying faults along which the greatest displacement has occurred.