標(biāo)題: Titlebook: Evolution of Geological Structures in Micro- to Macro-scales; S. Sengupta Book 1997 Springer Science+Business Media Dordrecht 1997 Deforma [打印本頁] 作者: DUBIT 時間: 2025-3-21 18:28
書目名稱Evolution of Geological Structures in Micro- to Macro-scales影響因子(影響力)
書目名稱Evolution of Geological Structures in Micro- to Macro-scales影響因子(影響力)學(xué)科排名
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書目名稱Evolution of Geological Structures in Micro- to Macro-scales網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Evolution of Geological Structures in Micro- to Macro-scales被引頻次
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書目名稱Evolution of Geological Structures in Micro- to Macro-scales年度引用學(xué)科排名
書目名稱Evolution of Geological Structures in Micro- to Macro-scales讀者反饋
書目名稱Evolution of Geological Structures in Micro- to Macro-scales讀者反饋學(xué)科排名
作者: 愛社交 時間: 2025-3-21 22:29 作者: 沒花的是打擾 時間: 2025-3-22 00:23 作者: nettle 時間: 2025-3-22 05:23 作者: 描繪 時間: 2025-3-22 12:23 作者: Acclaim 時間: 2025-3-22 13:21 作者: Acclaim 時間: 2025-3-22 19:06 作者: 合同 時間: 2025-3-23 00:05
Overthrust shear in mountain buildingformation is needed. This is the result of an analysis of a comprehensive data set, comprising fold axial plane and cleavage orientations, and finite and incremental strain. There is a tendency for the strain to be concentrated at the nappe boundaries. The orientation of the finite strain stretching作者: 異端邪說2 時間: 2025-3-23 01:49 作者: 無可非議 時間: 2025-3-23 06:07
Practical analysis of general shear zones using the porphyroclast hyperbolic distribution method: An76), among others. In general shear zones, rigid ellipsoidal grains may rotate either forwards (with the sense of shear) or backwards (counter to the sense of shear) according to their axial ratios and orientations. Grains of a critical shape have their forward motion exactly countered by backward m作者: Jogging 時間: 2025-3-23 12:17
Shear zones in foliated rocks: geometry and kinematics. These differences refer to:.In addition to this second point, the presence of a pre-existing foliation induces the development of minor structures arising from buckling instabilities formed at the marginal domains. These questions are reviewed and illustrated with examples taken from the Cap de Cr作者: Commonplace 時間: 2025-3-23 14:47
Development of compressional and extensional structures during progressive ductile shearing, Main Ceser Himachal Himalaya the MCTZ is well preserved in a half-klippe around the Chur peak. The ductile shearing related to the formation of the MCTZ was superimposed on strongly anisotropic metasedimentary rock sequences in which two phases of folding precede the ductile shearing event. Compressional s作者: CHURL 時間: 2025-3-23 19:38
Deformed lineation in ductile shear zones: a case study from the Proterozoic fold belt of Singhbhum,s. The commonly observed stretching lineation indicates the direction of movement. In most models of heterogeneous simple shear the C-surfaces are regarded as invariant, and remain planar during progressive deformation. However, it is well known that perturbations in the flow regime caused by slight作者: 禮節(jié) 時間: 2025-3-23 23:01
Construction and prospective use of displacement-difference vectors (DDVs) in vertical sections acroing actual DDV fields in deformed rock masses. This paper outlines a method of determining DDV rows which is tailored for use in partly eroded belts of ductile dip shear. The method employs arbitrary points on a strained material line coincident with the cross-sectional trace of the erosion surface.作者: 民間傳說 時間: 2025-3-24 05:38 作者: 祖?zhèn)髫敭a(chǎn) 時間: 2025-3-24 09:46
Strain and crystallographic fabric pattern in a folded calcite vein: the dependence on initial fabriing in the outer arc of a fold and layer-parallel shortening in the inner arc, with a neutral surface separating the two. We describe a folded fibrous calcite vein in which the primary crystallographic fabric, with c-axes perpendicular to the vein walls, allows only for layer shortening by twinning 作者: HEAVY 時間: 2025-3-24 14:29 作者: 砍伐 時間: 2025-3-24 18:02 作者: 除草劑 時間: 2025-3-24 20:33
Normal faulting and exhumation of metamorphic rocks in mountain beltslts in important crustal thickening and formation of high relief giving rise to intensive erosion. Erosional unloading causes the buoyant crustal slice to be exhumed at a rate comparable with the subduction rate..This process seems to work in different collisional belts explaining rapid syn-collisio作者: 指令 時間: 2025-3-25 00:32
Evolution of salients in a fold- and-thrust belt: the effects of sedimentary basin geometry, strain elf, lithotectonic stratigraphy of the sedimentary package, and deformation conditions (determined mainly by variations in the geothermal gradient). The differences in structural geometry and tectonic evolution between adjoining segments of the FTB result from broad variations in original taper, lit作者: 廣告 時間: 2025-3-25 05:01 作者: 繞著哥哥問 時間: 2025-3-25 10:12
Overthrust shear in mountain building shows again a swing to the west from the normal to the inverted limb directions, and rotates more rapidly than the finite strain fabric..A model consisting of overthrust shear zones is proposed. The shear zones occur in a top-downwards sequence analogous to thrust faults. Each shear zone starts bro作者: 地名詞典 時間: 2025-3-25 12:04
Practical analysis of general shear zones using the porphyroclast hyperbolic distribution method: Anvious assumptions of predominantly simple shear strain with .>1000 throughout nappe emplacement history. Changes in orientation of mafic dikes and deformed cross-bedded sandstones across the shear zone boundary allow us to use the general shear equation . = cot (θ ’) — ..cot(θ), where 7 is the shear作者: 賭博 時間: 2025-3-25 16:12
Development of compressional and extensional structures during progressive ductile shearing, Main Ce have developed during the same progressive ductile shear deformation and their development in a particular outcrop depends merely on the orientation of the layers with respect to the strain ellipsoid of the instantaneous flow field. Extensional structures in the Himalaya, as in other orogenic belts作者: Abjure 時間: 2025-3-26 00:02
Deformed lineation in ductile shear zones: a case study from the Proterozoic fold belt of Singhbhum,sity of deformation. The patterns have been theoretically deduced by applying simple shear deformation to gentle initial flexural perturbations. It has been demonstrated that at the initial stages of progressively increasing simple shear the deformed lineation is of Type 1 (l. ^ f. acute angle openi作者: Benzodiazepines 時間: 2025-3-26 02:03 作者: 有其法作用 時間: 2025-3-26 06:48 作者: 無法解釋 時間: 2025-3-26 09:44
Epitope Mapping by Antibody Competition,o describe the accumulation of displacement on faults, with recent models emphasizing the importance of fault interaction and other mechanical effects in causing variations in the displacement characteristics of faults. Faults have been shown to display power-law scaling relationships for displaceme作者: Truculent 時間: 2025-3-26 15:50 作者: confide 時間: 2025-3-26 18:39
Gianluigi Lichinchi,Tariq M. Ranaelf, lithotectonic stratigraphy of the sedimentary package, and deformation conditions (determined mainly by variations in the geothermal gradient). The differences in structural geometry and tectonic evolution between adjoining segments of the FTB result from broad variations in original taper, lit作者: Inordinate 時間: 2025-3-27 00:02
Signals and Communication Technologypagation folds reflects an apparent dip of the left lateral wall of the culmination. The available models also cannot adequately explain progressive growth of fault propagation folds in culmination zones or folded sequences. Application of the model in such curviplanar sequences leads to a locked si作者: Ballerina 時間: 2025-3-27 04:23 作者: Folklore 時間: 2025-3-27 09:20
https://doi.org/10.1007/978-3-319-52768-0vious assumptions of predominantly simple shear strain with .>1000 throughout nappe emplacement history. Changes in orientation of mafic dikes and deformed cross-bedded sandstones across the shear zone boundary allow us to use the general shear equation . = cot (θ ’) — ..cot(θ), where 7 is the shear作者: 無脊椎 時間: 2025-3-27 11:19 作者: 刪減 時間: 2025-3-27 15:11 作者: 災(zāi)難 時間: 2025-3-27 18:45
Experimental Biology and MedicineIt was also found that no correlation of rotation with aspect ratio could be detected for the observed aspect ratios between 1 and 3.5 in the experiment. An unexpected, isothermal coarsening of one of the crystalline phases in the system was observed in the high strain rate domain. The crystals coar作者: 培養(yǎng) 時間: 2025-3-28 00:49
Evolution of Geological Structures in Micro- to Macro-scales作者: 蛙鳴聲 時間: 2025-3-28 03:18
Evolution of Geological Structures in Micro- to Macro-scales978-94-011-5870-1作者: 亞當(dāng)心理陰影 時間: 2025-3-28 06:58 作者: Surgeon 時間: 2025-3-28 11:12 作者: 荒唐 時間: 2025-3-28 15:06
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.作者: 頭盔 時間: 2025-3-28 20:42 作者: Femish 時間: 2025-3-29 00:05
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.作者: STERN 時間: 2025-3-29 03:06
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.作者: 仲裁者 時間: 2025-3-29 10:32
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.作者: Neutropenia 時間: 2025-3-29 13:15
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.作者: dry-eye 時間: 2025-3-29 16:34 作者: 過剩 時間: 2025-3-29 23:22
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.作者: 淘氣 時間: 2025-3-30 01:36 作者: AMEND 時間: 2025-3-30 04:10
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.作者: hypnogram 時間: 2025-3-30 11:58
Book 1997s an overview ofnewly emerging concepts in a single volume. The book covers a widerange of advances in such broad fields as hydraulic factures, normalfaults, overthrusts, ductile shear zones, rock fabrics, folds,superposed folds and basement structures.作者: sperse 時間: 2025-3-30 12:57
d, provides an overview ofnewly emerging concepts in a single volume. The book covers a widerange of advances in such broad fields as hydraulic factures, normalfaults, overthrusts, ductile shear zones, rock fabrics, folds,superposed folds and basement structures.978-94-010-6481-1978-94-011-5870-1作者: 我要威脅 時間: 2025-3-30 20:32 作者: 外表讀作 時間: 2025-3-30 23:26
Imbricate thrust spacing: experimental and theoretical analysese thrust spacing increases to a maximum and then decreases down to a near-stable value. Thrust spacing shows a positive relationship with the dynamic factor, n. With increase in basal friction, thrust spacing decreases. Steepening of early frontal thrusts and formation of back-thrust also depend on the basal friction.作者: VOC 時間: 2025-3-31 01:11
