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compatible with evidence of high heat ow, elevated geotherms, and shallow asthenosphere Pre-rift volcanism is mostly calc-alkaline in composition Magmatism that accompanied extension is mostly basaltic Basalts from Nevada have an isotopic signature suggesting that they were derived from sublithospheric mantle This pattern matches evidence of mantle upwelling beneath the rift (Savage & Sheehan, 2000) 4 Small- and large-magnitude normal faulting Large extensional strains and thinning of the crust in wide rifts is partly accommodated by slip on normal faults Two contrasting patterns are evident First, the deformation can involve distributed normal faulting where a large number of more or less regularly spaced normal faults each accommodate a relatively small amount (<10 km) of the total extension Second, the strain may be highly localized onto a relatively small number of normal faults that accommodate large displacements of several tens of kilometers.

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Both patterns are common and may occur during different stages of rift evolution Many of the range-bounding normal faults in the Basin and Range record relatively small offsets These structures appear similar to those that characterize narrow rift segments Asymmetric half graben and footwall uplifts are separated by a dominant normal fault that accommodates the majority of the strain The morphology of these features is governed by the elastic properties of the lithosphere (Section 764) and the effects of syn-rift sedimentation and erosion The asymmetry of the half graben and the dips of the range-bounding faults also commonly change in adjacent basin-range pairs Many of the tectonically active faults maintain steep dips (>45 ) that may penetrate through the upper crust However, unlike the border faults of East Africa, some of the rangebounding faults of the Basin and Range exhibit geometries that involve low-angle extensional detachment faults.

A few of these low-angle normal faults accommodate very large displacements and penetrate tens of.

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Table 13.4: Maximum Free-Distance Trellis Codes for Amplitude Modulated (OneDimensional) Constellations [347]

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