2 – JOINTS AND SHEAR FRACTURES IN ROCK
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[1] Leon M Keer,et al. Unstable growth of thermally induced interacting cracks in brittle solids , 1978 .
[2] R. Kranz,et al. Crack-crack and crack-pore interactions in stressed granite , 1979 .
[3] David D. Pollard,et al. Field relations between dikes and joints: Emplacement processes and paleostress analysis , 1986 .
[4] T. Engelder. Loading paths to joint propagation during a tectonic cycle: an example from the Appalachian Plateau, U.S.A. , 1985 .
[5] Michael P. Ryan,et al. Cyclic fracture mechanisms in cooling basalt , 1978 .
[6] D. Bahat. A "giant" plumose marking in paleozoic sandstones from Sinai , 1980 .
[7] T. Engelder,et al. On the use of regional joint sets as trajectories of paleostress fields during the development of the Appalachian Plateau, New York , 1980 .
[8] W. Z. Savage. The development of residual stress in cooling rock bodies , 1978 .
[9] Mark D. Zoback,et al. In situ stress, natural fracture distribution, and borehole elongation in the Auburn Geothermal Well, Auburn, New York , 1985 .
[10] William W Rubey,et al. ROLE OF FLUID PRESSURE IN MECHANICS OF OVERTHRUST FAULTING I. MECHANICS OF FLUID-FILLED POROUS SOLIDS AND ITS APPLICATION TO OVERTHRUST FAULTING , 1959 .
[11] David L. Smith,et al. Diffusional crack healing in quartz , 1984 .
[12] M. L. Sbar,et al. The relationship betweenin situ strain relaxation and outcrop fractures in the Potsdam Sandstone, Alexandria Bay, New York , 1977 .
[13] D. Pollard,et al. Formation and interpretation of dilatant echelon cracks , 1982 .
[14] D. Weaire,et al. A new model for the Giant's Causeway , 1983, Nature.
[15] S. Kirby,et al. Transient creep and semibrittle behavior of crystalline rocks , 1978 .
[16] J. Logan,et al. Microscopic Feather Fractures , 1970 .
[17] Gary L. Foote,et al. Joint orientation in Devonian rocks in the northern portion of the lower peninsula of Michigan , 1981 .
[18] F. Walker. Differentiation of the Palisade diabase, New Jersey , 1940 .
[19] G. Eisbacher,et al. Elastic strain recovery in Proterozoic rocks near Elliot Lake, Ontario , 1971 .
[20] C. Roering. The geometrical significance of natural en-echelon crack-arrays , 1968 .
[21] P. Hancock. The analysis of en-échelon veins , 1972, Geological Magazine.
[22] T. Engelder,et al. Surface morphology on cross-fold joints of the Appalachian Plateau, New york and Pennsylvania , 1984 .
[23] D. Bahat. Theoretical considerations on mechanical parameters of joint surfaces based on studies on ceramics , 1979, Geological Magazine.
[24] A. Beach,et al. The geometry of en-echelon vein arrays , 1975 .
[25] M. Friedman,et al. Microscopic feather fractures in the faulting process , 1976 .
[26] Arvid M. Johnson,et al. Development of faults as zones of deformation bands and as slip surfaces in sandstone , 1978 .
[27] B. Atkinson. Subcritical crack growth in geological materials , 1984 .
[28] M. Etheridge. Differential stress magnitudes during regional deformation and metamorphism: Upper bound imposed by tensile fracturing , 1983 .
[29] E. Yoffe,et al. LXXV. The moving griffith crack , 1951 .
[30] Z. Reches. Analysis of faulting in three-dimensional strain field , 1978 .
[31] W. Durham,et al. Mechanisms of crack growth in quartz , 1975 .
[32] P. L. Hancock,et al. Brittle microtectonics: principles and practice , 1985 .
[33] R. Rispoli. Stress fields about strike-slip faults inferred from stylolites and tension gashes , 1981 .
[34] A. Nur,et al. Granites: Relation of Properties in situ to Laboratory Measurements , 1968, Science.
[35] Jointing in the coal beds of Ohio , 1942 .
[36] J. Handin,et al. Fracture-surface energy of rocks , 1972 .
[37] D. G. Holloway,et al. On the shape and size of the fracture zones on glass fracture surfaces , 1966 .
[38] H. Wang,et al. Microcracks in crystalline rock from 5.3‐km depth in the Michigan Basin , 1978 .
[39] G. Simmons,et al. Characteristics of microcracks in amphibolite and granulite facies grade rocks from southeastern Pennsylvania , 1982 .
[40] D. Wise. Microjointing in Basement, Middle Rocky Mountains of Montana and Wyoming , 1964 .
[41] J. T. Engelder,et al. Cataclasis and the Generation of Fault Gouge , 1974 .
[42] E. Z. Lajtai. A theoretical and experimental evaluation of the Griffith theory of brittle fracture , 1971 .
[43] A. Beach. Vein arrays, hydraulic fractures and pressure-solution structures in a deformed flysch sequence S.W. England , 1977 .
[44] A. McGarr. Some constraints on levels of shear stress in the crust from observations and theory , 1980 .
[45] C. H. Scholz,et al. Mechanism of creep in brittle rock , 1968 .
[46] D. Lockner,et al. Acoustic emission and creep in rock at high confining pressure and differential stress , 1977 .
[47] E. Yoffe,et al. The moving Griffith crack , 1951 .
[48] John G. Ramsay,et al. The crack–seal mechanism of rock deformation , 1980, Nature.
[49] M. L. Sbar,et al. Near-surface in situ stress: 2. A comparison with stress directions inferred from earthquakes, joints, and topography near Blue Mountain Lake, New York , 1984 .
[50] P. Gash. A study of surface features relating to brittle and semibrittle fracture , 1971 .
[51] Paul Segall,et al. Joint formation in granitic rock of the Sierra Nevada , 1983 .
[52] A. Spry. The origin of columnar jointing, particularly in basalt flows , 1962 .
[53] T. Engelder. Is there a genetic relationship between selected regional joints and contemporary stress within the lithosphere of North America , 1982 .
[54] F. Donath. Analysis of Basin-Range Structure, South-Central Oregon , 1962 .
[55] C. Wentworth,et al. Intrusive Rocks of the Leeward Slope of the Koolau Range, Oahu , 1940, The Journal of Geology.
[56] G. MacDonald. Chapter 1: Orientation of Anisotropic Minerals in a Stress Field , 1960 .
[57] A. Thompson,et al. Regional Geophysics of the Basin and Range Province , 1974 .
[58] E. Z. Lajtai. Mechanics of Second Order Faults and Tension Gashes , 1969 .
[59] T. Engelder,et al. Mesoscopic fault array of the northern Umbrian Apennine fold belt, Italy: Geometry of conjugate shear by pressure-solution slip , 1982 .
[60] R. P. Nickelsen,et al. Jointing in the Appalachian Plateau of Pennsylvania , 1967 .
[61] K. V. Steeg. Some Structural Features of Ohio , 1944, The Journal of Geology.
[62] W. F. Brace,et al. A note on brittle crack growth in compression , 1963 .
[63] R. A. Hodgson,et al. Classification of structures on joint surfaces , 1961 .
[64] James B. Anderson,et al. Topological properties of random crack networks , 1976 .
[65] J. J. Gallagher,et al. Experimental studies relating to microfracture in sandstone , 1974 .
[66] H. C. Heard,et al. Prediction of elastic moduli via crack density in pressurized and thermally stressed rock , 1985 .
[67] J. Parker. Regional systematic jointing in slightly deformed sedimentary rocks , 1942 .
[68] T. Engelder. Reply to “Comment on ‘Is there a genetic relationship between selected regional joints and contemporary stress within the lithosphere of North America?’” , 1982 .
[69] L. Rixon,et al. Stress configurations in conjugate quartz-vein arrays , 1983 .
[70] O. F. Tuttle. Structural Petrology of Planes of Liquid Inclusions , 1949, The Journal of Geology.
[71] P. Segall. Formation and growth of extensional fracture sets , 1984 .
[72] V. E. Shainin. CONJUGATE SETS OF EN ECHELON TENSION FRACTURES IN THE ATHENS LIMESTONE AT RIVERTON, VIRGINIA , 1950 .
[73] D. Secor. Role of fluid pressure in jointing , 1965 .
[74] R. Kranz. Microcracks in rocks: a review , 1983 .
[75] A. Lachenbruch. Mechanics of Thermal Contraction Cracks and Ice-Wedge Polygons in Permafrost , 1962 .
[76] G. Oertel. The mechanism of faulting in clay experiments , 1965 .
[77] J. C. Roberts. Feather-fracture, and the mechanics of rock-jointing , 1961 .