Stable isotope geochemistry and examination of meso- and microstructures show that strain conditions differed through the course of tectonic history. Carbon and oxygen isotope analyses of the calcite-filled extensional fractures, the sigmoidal veins present between stylolitic cleavage surfaces, and fault plane surfaces with differing motion, demonstrate those different geneses. -from Authors

Maiorani, A., Funiciello, R., Mattei, M., Turi, B. (1992). Stable isotope geochemistry and structural elements of the Sabina region (Central Apennines, Italy). TERRA NOVA, 4(4), 484-488.

Stable isotope geochemistry and structural elements of the Sabina region (Central Apennines, Italy)

Funiciello, R.;Mattei, M.;
1992-01-01

Abstract

Stable isotope geochemistry and examination of meso- and microstructures show that strain conditions differed through the course of tectonic history. Carbon and oxygen isotope analyses of the calcite-filled extensional fractures, the sigmoidal veins present between stylolitic cleavage surfaces, and fault plane surfaces with differing motion, demonstrate those different geneses. -from Authors
1992
Maiorani, A., Funiciello, R., Mattei, M., Turi, B. (1992). Stable isotope geochemistry and structural elements of the Sabina region (Central Apennines, Italy). TERRA NOVA, 4(4), 484-488.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11590/435347
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