Structural geology (English Wikipedia)

Analysis of information sources in references of the Wikipedia article "Structural geology" in English language version.

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Livaccari, Richard F.; Burke, Kevin; Scedilengör, A. M. C. (1981). "Was the Laramide orogeny related to subduction of an oceanic plateau?". Nature. 289 (5795): 276–278. Bibcode:1981Natur.289..276L. doi:10.1038/289276a0. S2CID 27153755.
V. Guerriero; et al. (2011). "Improved statistical multi-scale analysis of fractures in carbonate reservoir analogues". Tectonophysics. 504 (1). Elsevier: 14–24. Bibcode:2011Tectp.504...14G. doi:10.1016/j.tecto.2011.01.003. V. Guerriero; et al. (2009). "Quantifying uncertainties in multi-scale studies of fractured reservoir analogues: Implemented statistical analysis of scan line data from carbonate rocks". Journal of Structural Geology. 32 (9). Elsevier: 1271–1278. Bibcode:2010JSG....32.1271G. doi:10.1016/j.jsg.2009.04.016.

Livaccari, Richard F.; Burke, Kevin; Scedilengör, A. M. C. (1981). "Was the Laramide orogeny related to subduction of an oceanic plateau?". Nature. 289 (5795): 276–278. Bibcode:1981Natur.289..276L. doi:10.1038/289276a0. S2CID 27153755.
V. Guerriero; et al. (2011). "Improved statistical multi-scale analysis of fractures in carbonate reservoir analogues". Tectonophysics. 504 (1). Elsevier: 14–24. Bibcode:2011Tectp.504...14G. doi:10.1016/j.tecto.2011.01.003. V. Guerriero; et al. (2009). "Quantifying uncertainties in multi-scale studies of fractured reservoir analogues: Implemented statistical analysis of scan line data from carbonate rocks". Journal of Structural Geology. 32 (9). Elsevier: 1271–1278. Bibcode:2010JSG....32.1271G. doi:10.1016/j.jsg.2009.04.016.

Russell, William L (1955). "1. Introduction". Structural Geology for Petroleum Geologists. New York: McGraw-Hill. p. 1.

Livaccari, Richard F.; Burke, Kevin; Scedilengör, A. M. C. (1981). "Was the Laramide orogeny related to subduction of an oceanic plateau?". Nature. 289 (5795): 276–278. Bibcode:1981Natur.289..276L. doi:10.1038/289276a0. S2CID 27153755.