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Science
The McGraw-Hill Companies
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Why joints are more abundant than faults. A conceptual model ...
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Suspa Sinha & G. Ian Alsop & T.K. Biswal (...)
Tertiary compressional overprint on Aptian–Albian extensional ...
Bele? n Oliva-Urcia & Teresa Roma? n-Berdiel & Antonio M. Casas & Emilio L. Pueyo (...)
Stylolites in limestone: Magnitude of contractional strain accommodated ...
Antonio Benedicto & Richard A. Schultzb
Stylolite interfaces and surrounding matrix material: Nature ...
Marcus Ebner & Sandra Piazolo & Francois Renard & Daniel Koehn (...)
Structural geometry of an exhumed UHP terrane in the eastern ...
Lu Wang & Timothy M. Kusky & Sanzhong Li (...)
Structural and petrophysical evolution of extensional fault ...
F. Balsamo & F. Storti & F. Salvini & A.T. Silva (...)
Strain pattern within and around denser blocks sinking within ...
Stef? Burchardt & Hemin Koyi & Harro Schmeling (...)
Static recrystallization of vein quartz pebbles in a high-pressure ...
Claudia Trepmann & Annette Lenze & Bernhard Stöckhert (...)
Sequential deformation from serpentinite mylonite to metasomatic ...
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Sequence Stratigraphy
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Sedimentary Processes: Particle-Driven Subaqueous Gravity Processes
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Scaling relationships between stratabound pressure solution ...
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Rocks and Minerals
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Recognizing soft-sediment structures in deformed rocks of orogens
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Quantifying uncertainties in multi-scale studies of fractured ...
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