Preliminary stress measurements in central California using the hydraulic fracturing technique

Author:

Zoback Mark D.,Healy John H.,Roller John C.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference21 articles.

1. Aamodt, R. L. (1974),An experimental measurement of in situ stress in granite by hydraulic fracturing, Los Alamos Scientific Laboratory Report 5605-MS.

2. Bredehoeft, J. D., Wolff, R. G., Keys, W. S. andShuter, E. (1976),Hydraulic fracturing to determine the regional in situ field, Picenace Basin, Colorado, Geol. Soc. Amer. Bull.87, 250–258.

3. Durham, D. L. (1974),Groundwater geology of the southern Salinas valley area, California, U.S. Geological Survey Prof. Paper819, 111 pp.

4. Ford, R. S.,Groundwater geology of Livermore valley — a satellite urban area inUrban Environmental Geology in the San Francisco Bay Region (ed. E. A. Daneby) (San. Fran. Section Assoc. of Engl. Geol., 1969), 162 pp.

5. Haimson, B. C. andFairhurst, C.,In situ stress determination at great depth by means of hydraulic fracturing inRock Mech. Theory and Practice, Proc. of 11th Symp. of Rock Mech. Univ. of Ca., Berkeley, CA., June 1969 (ed. W. H. Somerton) (Soc. Mining Eng. AIME, New York, 1970).

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