Zobrazeno 1 - 10
of 11
pro vyhledávání: '"M. A. Chinnery"'
Autor:
M. A. Chinnery
Publikováno v:
Bulletin of the Seismological Society of America. 53:921-932
In a previous paper (Chinnery, 1961) an investigation of the deformation of the ground around a strike-slip fault was described. This work is now extended to a calculation of the change in stress distribution that is brought about by such a fault. Co
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::375ebef0693b528d3698b4f41394fa68
https://doi.org/10.1785/bssa0530050921
https://doi.org/10.1785/bssa0530050921
Autor:
M. A. Chinnery
Publikováno v:
Canadian Journal of Earth Sciences. 3:175-190
A secondary fault is defined as a fracture which arises as a direct result of movement on a master transcurrent fault. Some previous approaches to the study of secondary faulting are discussed, and fallacies in the arguments of McKinstry (1953) and M
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b345640afd3a733fb29b4c3abcdebdba
https://doi.org/10.1139/e66-014
https://doi.org/10.1139/e66-014
Autor:
M. A. Chinnery
Publikováno v:
Journal of Geophysical Research. 69:2085-2089
Recent theoretical expressions for the change in stress distribution caused by strike-slip faulting are applied to five real faults, and estimates are made of the maximum shear stress relieved in each case. The calculated values lie between 107 and 1
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::58407beebc1b40a35e31790fb2b1f458
https://doi.org/10.1029/jz069i010p02085
https://doi.org/10.1029/jz069i010p02085
Publikováno v:
Canadian Journal of Earth Sciences. 2:418-424
The Red Lake greenstone belt is Archaean in age (older than 2.5 billion years) and is located in the Superior province of the Canadian Precambrian Shield. It is a fairly typical greenstone belt, being composed of a complex assemblage of lavas, sedime
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::28ec072429eb33f494f3a36f40c9f782
https://doi.org/10.1139/e65-036
https://doi.org/10.1139/e65-036
Autor:
M. A. Chinnery
Publikováno v:
Bulletin of the Seismological Society of America. 51:355-372
A rectangular dislocation surface (i.e., a surface across which there is a discontinuity in the displacement vector) is used as a model of a vertical transcurrent fault. The results of Steketee (1958a) are employed to derive, in analytical form, the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e88f951b35d5579dbe06cb7d4b667ff0
https://doi.org/10.1785/bssa0510030355
https://doi.org/10.1785/bssa0510030355
Autor:
M. A. Chinnery
Publikováno v:
GEOPHYSICS. 26:480-489
A method is given for the calculation of terrain corrections for airborne measurements of the vertical gradient of gravity. This includes a short account of the theory concerned, a description of the practical procedure, a complete set of numerical t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5c1a30ea177603c6af0c8f43b1301cd3
https://doi.org/10.1190/1.1438901
https://doi.org/10.1190/1.1438901
Autor:
M. A. Chinnery
Publikováno v:
Canadian Journal of Earth Sciences. 3:163-174
The results of two previous papers by Chinnery published in 1963 and 1964 are used to calculate the distribution of stress that is present after the formation of a strike-slip fault. The pattern obtained shows that although the initial stress is redu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8487d9a4029fac68edaf17f4ede996af
https://doi.org/10.1139/e66-013
https://doi.org/10.1139/e66-013
Autor:
M. A. Chinnery
Publikováno v:
Journal of Geophysical Research. 70:4627-4632
The results of an earlier paper (Chinnery, 1961) are used in this discussion of the nature of the vertical displacements that should accompany movement on a transcurrent fault. In spite of the inadequacies of the model, it is shown that the uplift an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fa3e435c9d2908c508e8f1dc1bb53ce3
https://doi.org/10.1029/jz070i018p04627
https://doi.org/10.1029/jz070i018p04627
Autor:
M. A. Chinnery
Publikováno v:
Journal of Geophysical Research. 65:3852-3854
There has been considerable discussion in recent years of the kind of stress changes that occur at the focus of an earthquake as fracture takes place. Two mechanisms consisting of stress patterns in the form of a single couple with moment (nucleus I)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::97d4046c4b3eaeff16dbe53218558691
https://doi.org/10.1029/jz065i011p03852
https://doi.org/10.1029/jz065i011p03852
