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![Bulletin of the Geological Society of America. Geology. 178 REID ET AL. REPORT OX NOMENCLATURE OF FAULTS. Figure reverse Fault due to an oolique Slip. determined by the displacement of the Bulletin of the Geological Society of America. Geology. 178 REID ET AL. REPORT OX NOMENCLATURE OF FAULTS. Figure reverse Fault due to an oolique Slip. determined by the displacement of the](https://c8.alamy.com/comp/RGGTWG/bulletin-of-the-geological-society-of-america-geology-178-reid-et-al-report-ox-nomenclature-of-faults-figure-reverse-fault-due-to-an-oolique-slip-determined-by-the-displacement-of-the-stratum-has-caused-an-extension-at-right-angles-to-the-fault-strik-it-is-evident-that-if-the-hanging-wall-had-moved-as-in-figure-8-with-the-stratum-dipping-as-there-represented-we-should-have-had-a-normal-fault-and-a-contraction-at-right-angles-to-the-fault-strike-the-relations-of-the-two-parts-of-the-disrupted-stratum-in-fig-ure-7-are-exactly-the-same-as-if-we-had-had-a-simple-reverse-dip-slip-fa-RGGTWG.jpg)