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Product Code: FLD046 (Field Guide 46)
It contains a Cambrian-Ordovician carbonate platform that shares many characteristics with coeval sedimentary rocks of Laurentia
and establishes links to exhumed sediment source areas in a plausible paleogeographic framework
The first symposium on the Cenozoic basins of the Death Valley region includes 16 papers that provide a major updating on the structural and stratigraphic features and chronology of the principal basins
and satellites
Gneiss Domes in Orogeny 1-1-001-337-4330-337 Product Code: FLD046 (Field GuideEditors: Donna L. Whitney, Christian Teyssier, and Christine S. Siddoway Buy the e book (not available in print) Domal structures cored by high grade metamorphic rocks and granite occur in every exhumed mountain belt worldwide, representing orogenic events from the Archean to the present. Field relationships, thermal histories, and results of modeling of these structures show that dome emplacement and orogenesis are intimately related. Flow of crust
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