 The fault strike is the direction of the intersection of the fault surface, or the shear zone, with a horizontal plane. The fault dip is the inclination of the fault surface, or shear zone, measured from a horizontal plane.  Mineral Deposits - Página 132por Waldemar Lindgren - 1913 - 883 páginasVista completa - Acerca de este libro
 | Geological Society of America - 1913 - 850 páginas
...horse is a mass of rock broken from one wall and caught between the walls of the fault. (See figure 1.) The fault strike is the direction of the intersection...inclination of the fault surface, or shear zone, measured downward from a horizontal plane. It is never greater than 90 degrees. The hade is the inclination... | |
 | William Harvey Emmons - 1918 - 642 páginas
...will suffice, and even then it is not always possible to locate the other end of the faulted body. The fault strike is the direction of the intersection of the fault surface with a horizontal plane—that is, a level line along a fault. The fault dip is the inclination of... | |
 | Albert Hill Fay - 1920 - 770 páginas
...(Power) Fault space. The space between the walls of an open fault. (Lindgren, p. 117) Fault strike. The direction of the Intersection of the fault surface, or the shear zone, with a horizontal surface. (Lindgren, p. 118) Fault surface. The surface along which dislocation has taken place. May... | |
 | David Talbot Day - 1922 - 988 páginas
...lit plane.—A surface along which dislocation or faulting has taken place (Kay). lit strike.—The direction of the intersection of the fault surface, or the shear zone, with a horizontal surface (Lindgren). lit terrace.—A terrace formed by two parallel fault scarps on the same declivity,... | |
 | William Harvey Emmons - 1922 - 544 páginas
...shown that one or the other wall has been moved along the fracture plane (see Figs. 144, 145, 146). The fault strike is the direction of the intersection of the fault surface with a horizontal plane—that is, a level line along a fault plane. The fault dip is the inclination... | |
 | William Harvey Emmons - 1922 - 544 páginas
...shown that one or the other wall has been moved along the fracture plane (see Figs. 144, 145, 146). The fault strike is the direction of the intersection of the fault surface with a horizontal plane—that is, a level line along a fault plane. The fault dip is the inclination... | |
 | Erhard Winkler - 1997 - 340 páginas
...rock due to the friction of the two walls of a fault rubbing against each other (AGI). Fault strike. The direction of the intersection of the fault surface, or the shear zone, with a horizontal plane (AG!). Felsite. An igneous rock with or without phenocrysts, in which either the whole or the groundmass... | |
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