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The Global ETD Search service is a free service for researchers
to find electronic theses and dissertations. This service is
provided by the
Networked Digital Library of Theses and Dissertations.
Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
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Showing 101 to 105 of 105 (0.107 seconds)Spelling suggestions: "subject:"dock deformation"" "subject:"rock deformation""
| 101 |
Deformation in foreland basins of the western Alps ( Pelvoux massif, SE France ); significance for the development of the Alpine ARCBürgisser, Judith 02 February 1998 (has links) (PDF)
pas de résumé
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| 102 |
Style of deformation of upper plate rocks of the San Manuel-Camp Grant low-angle normal fault system, Black Hills, Pinal County, ArizonaHansen, Jerome Brian January 1983 (has links)
No description available.
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| 103 |
Kinematic analysis of deformation at the margin of a regional shear zone, Buehman Canyon area, Santa Catalina Mountains, ArizonaBykerk-Kauffman, Ann, Bykerk-Kauffman, Ann January 1983 (has links)
No description available.
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| 104 |
Effect of partial melting on lattic preferred orientations in two common foliated felsic rocksRazo, Maria patricia 02 May 2023 (has links)
No description available.
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| 105 |
Structural Investigations of the Italian Trap Allochthon, Redington Pass, Pima County, ArizonaBenson, Gregory Scott January 1981 (has links)
Italian Trap Allochthon is a rare upper-plate exposure of Paleozoic metasedimentary and Precambrian to Tertiary crystalline tectonites in the Santa Catalina-Rincon metamorphic core complex. Elsewhere in the complex, metasedimentary tectonite is usually restricted to an autochthononous position. The internal structures of the allochthon consist of numerous low-angle faults, tear faults, and overturned asymmetric and upright folds. Close association of the low-angle faults and asymmetric folds, and vergence of the folds, indicates that these folds were formed during westward transport along the low-angle faults. The structures of the allochthon are truncated and rotated to the northeast by a listric (?) normal fault. The probable shape of the fault surface, together with the northeastward rotation of the internal structures, suggests translation of the allochthon from the northeast to the southwest. The fact that metasedimentary tectonites are found in upper- plate position indicates that the listric (?) normal faulting post-dates the metamorphism of the Paleozoic and Mesozoic strata. Metamorphism in turn was part of the development of the Santa Catalina-Rincon metamorphic core complex. It is inferred that the Italian Trap Allochthon was emplaced in the final stages of profound regional extension which prevailed during the mid-Tertiary in southern Arizona.
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