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The 1957 Gobi-Altay earthquake is the last major earthquake (M ~ 8) to occur in a continental region
including excellent examples of geomorphology
It contains a Cambrian-Ordovician carbonate platform that shares many characteristics with coeval sedimentary rocks of Laurentia
Pages: 436
Gneiss Domes in Orogeny 1-1-001-337-4330-337 The 1957 Gobi-Altay earthquake isEditors: 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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