Titlebook: Evolution of Geological Structures in Micro- to Macro-scales; S. Sengupta Book 1997 Springer Science+Business Media Dordrecht 1997 Deforma

荒唐

Epos Word, Narrative and the Iliads considered to be related to a combination of lateral downcutting of the Moine thrust and crustal duplication of the Moine sequence with, in the north, emplacement of rocks of lower crustal origin. Such a structure is reflected in the geometry of the Moine outcrop.

頭盔

Femish

Ellen Kilger,Wolfgang Hammerschmidtthe belt boundaries. Strongly divergent DDVs suffice for eliminating the possibility of finite simple shear, but rows of virtually parallel DDVs are difficult to interpret. This is illustrated in a two-dimensional structural model containing a pair of dip-shear zones.

STERN

Frank B. Furnari,Joseph S. Paganoin to the inner edge, suggesting that a neutral surface existed at the outer edge. This is supported by approximate measurements of twinning strain that show a strain gradient consistent with TLS, and that indicate also about 10% layer-parallel shortening prior to fold growth.

仲裁者

Construction and prospective use of displacement-difference vectors (DDVs) in vertical sections acrothe belt boundaries. Strongly divergent DDVs suffice for eliminating the possibility of finite simple shear, but rows of virtually parallel DDVs are difficult to interpret. This is illustrated in a two-dimensional structural model containing a pair of dip-shear zones.

Neutropenia

Strain and crystallographic fabric pattern in a folded calcite vein: the dependence on initial fabriin to the inner edge, suggesting that a neutral surface existed at the outer edge. This is supported by approximate measurements of twinning strain that show a strain gradient consistent with TLS, and that indicate also about 10% layer-parallel shortening prior to fold growth.

dry-eye

過剩

Introduction The book is divided in five broad sections: Part One, Fractures, faults and nappes; Part Two, Ductile shear zones; Part Three, Fabric; Part Four, Folds and superposed folds; Part Five, Basement structures. There is a certain amount of overlapping of these topics, especially where a tectonic synthesis of a large orogenic unit has been made.

淘氣

AMEND

Shear zones in foliated rocks: geometry and kinematicsrising from buckling instabilities formed at the marginal domains. These questions are reviewed and illustrated with examples taken from the Cap de Creus in the Hercynian basement of the easternmost Pyrenees.