scholarly journals In situ geomechanics of crystalline and sedimentary rocks; Part IV, An update on two BASIC computer programs for the determination of in situ stresses using the CSIRO hollow inclusion stress cell and the USBM borehole deformation gage

1985 ◽  
Author(s):  
H.S. Swolfs ◽  
P.S. Powers
1972 ◽  
Vol 98 (1) ◽  
pp. 169-169
Author(s):  
Merlin D. Copen ◽  
George B. Wallace

1970 ◽  
Vol 7 (2) ◽  
pp. 576-578
Author(s):  
G. H. Elsbacher ◽  
H. U. Bielenstein

In situ stresses obtained by measurements of elastic – strain – recovery in quartzose sedimentary rocks near Elliot Lake are interpreted in terms of two stress environments: one stress field induced by mining close to the mine openings and a remanent stress field preserved in the rocks from a time of tectonic deformation in the area.


1983 ◽  
Vol 105 (2) ◽  
pp. 125-127 ◽  
Author(s):  
W. E. Warren

Several problems in analysis can arise in estimating in-situ stresses from standard hydraulic fracturing operations if the borehole is not aligned with one of the principal stress directions. In these nonaligned situations, the possibility of fracturing a spherical cavity for estimating the in-situ stresses is investigated. The theory utilizes all the advantages of direct stress measurements associated with hydraulic fracturing and eliminates the geometrical problems associated with the analysis of hydraulic fractures in cylindrical boreholes.


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