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FeO, Fe<jats:sub>8.0<\/jats:sub>, and   Tb\/Yb increase, whereas Si<jats:sub>8.0<\/jats:sub> and Al<jats:sub>8.0<\/jats:sub> decrease,   from west to east across the B&amp;R along a profile at   36\u00b0\u201337\u00b0N. These variations are qualitatively consistent   with shallower melting beneath the Western Great Basin (WGB) than in the central   B&amp;R. In order to quantify the depth range and percent of decompression   melting, we invert primary Na<jats:sub>2<\/jats:sub>O and FeO contents of basalts using a   melting model based on the partitioning of FeO and MgO in olivine and   Na<jats:sub>2<\/jats:sub>O in clinopyroxene. An independent inversion, using the rare   earth elements (REE), corroborates the melting depths obtained from the major   element model and places most of the melting beneath the central B&amp;R in the   garnet\u2010peridotite stability field. We find that the shape of the melting region   across the B&amp;R closely mimics the shape of the mantle lithosphere, as   inferred from geological and geophysical observations. Melting across the study area   occurs largely within the asthenosphere and generally stops at the base of the   mantle lithosphere. In the WGB, melting paths are shallow, from 75 to 50 km, and in   some cases extend almost to the base of the crust. These melting paths are   consistent with adiabatic melting in normal\u2010temperature asthenosphere, beneath an   extensively thinned (or absent) mantle lithosphere. Shallow melting is consistent   with geobarometry and isotopic compositions of local mantle xenoliths. Lithospheric   thinning was caused by thermal erosion during Mesozoic subduction and\/or simple   shear or foundering during Cenozoic extension. In contrast, melting beneath the   central B&amp;R occurs beneath thick mantle lithosphere and requires mantle   potential temperatures 200\u00b0C hotter than normal (melting paths from 140 to   100 km). The excess temperature beneath the central B&amp;R is consistent with   active upwelling of hot mantle in this region.<\/jats:p>","DOI":"10.1029\/2001jb000209","type":"journal-article","created":{"date-parts":[[2002,10,27]],"date-time":"2002-10-27T18:39:25Z","timestamp":1035743965000},"source":"Crossref","is-referenced-by-count":262,"title":["A mantle melting profile across the Basin and Range, SW USA"],"prefix":"10.1029","volume":"107","author":[{"given":"K.","family":"Wang","sequence":"first","affiliation":[{"name":"Department of Geology University of Kansas  Lawrence Kansas USA"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"T.","family":"Plank","sequence":"additional","affiliation":[{"name":"Department of Earth Sciences Boston University  Boston Massachusetts USA"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"J. 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