標(biāo)題: Titlebook: Experimental and Natural Rock Deformation / Experimentelle und natürliche Gesteinsverformung; Proceedings of the I Peter Paulitsch Conferen [打印本頁] 作者: 黑暗社會 時間: 2025-3-21 18:06
書目名稱Experimental and Natural Rock Deformation / Experimentelle und natürliche Gesteinsverformung影響因子(影響力)
書目名稱Experimental and Natural Rock Deformation / Experimentelle und natürliche Gesteinsverformung影響因子(影響力)學(xué)科排名
書目名稱Experimental and Natural Rock Deformation / Experimentelle und natürliche Gesteinsverformung網(wǎng)絡(luò)公開度
書目名稱Experimental and Natural Rock Deformation / Experimentelle und natürliche Gesteinsverformung網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Experimental and Natural Rock Deformation / Experimentelle und natürliche Gesteinsverformung被引頻次
書目名稱Experimental and Natural Rock Deformation / Experimentelle und natürliche Gesteinsverformung被引頻次學(xué)科排名
書目名稱Experimental and Natural Rock Deformation / Experimentelle und natürliche Gesteinsverformung年度引用
書目名稱Experimental and Natural Rock Deformation / Experimentelle und natürliche Gesteinsverformung年度引用學(xué)科排名
書目名稱Experimental and Natural Rock Deformation / Experimentelle und natürliche Gesteinsverformung讀者反饋
書目名稱Experimental and Natural Rock Deformation / Experimentelle und natürliche Gesteinsverformung讀者反饋學(xué)科排名
作者: Insubordinate 時間: 2025-3-22 00:12 作者: Hyperlipidemia 時間: 2025-3-22 03:25 作者: DEVIL 時間: 2025-3-22 05:26
über die Verwendbarkeit der Anisotropie der Magnetischen Suszeptibilit?t zur Bestimmung der MagnetitThe present paper deals with using of anisotropy of magnetic susceptibility to the determination of dimensional orientation of magnetite in rocks. As an example of practical application of this method some results for Blansko — type granodiorite from Brno massif are presented.作者: LIEN 時間: 2025-3-22 09:31
Regelungseigenschaften Monomineralischer Gesteine bei Gerichteter BeanspruchungIn a hydrostatic stressfield mineral grains do not show any preferred orientation. In uniaxial stress we will expect preferred orientation for the crystallites. With optical and electrical methods the preferred orientation of experimental deformed calcite and quartz were determined.作者: 做作 時間: 2025-3-22 14:40 作者: 做作 時間: 2025-3-22 19:08
https://doi.org/10.1007/978-3-642-95187-9Deformation; Gestein; formation; mineral; mineralogy; petrology作者: TEN 時間: 2025-3-23 00:17 作者: GEM 時間: 2025-3-23 01:55 作者: 能夠支付 時間: 2025-3-23 08:22 作者: 考古學(xué) 時間: 2025-3-23 11:41 作者: 吼叫 時間: 2025-3-23 16:26
https://doi.org/10.1007/978-3-658-11867-90 Jahren wegen seiner gro?en Bedeutung für Forschung und technische Anwendung eine weite Verbreitung erfahren. Der Einsatz des Verfahrens war jedoch infolge des relativ gro?en Zeitbedarfs für eine solche Texturbestimmung und vor allem für die Auswertung der Ergebnisse begrenzt. Eine wesentlich schne作者: Spartan 時間: 2025-3-23 18:45
Managing Surges of Capital Flows, schists garnets (110) lie generally parallel to the (ab)-plane of the fabric; in only one case (111) was parallel to (ab)..In mesozonal rocks, eclogites and one granulite, garnets (100) show a preferred orientation // ab; (100) lies in one case // ac..The kinematic axes of the rocks were confirmed 作者: 使服水土 時間: 2025-3-24 00:51
Social Welfare and Competitivenessals. The composite specimens were elongated by various amounts under a confining pressure of 5 kilobars and a temperature, in most cases, of 300 °C. A detailed microscopic study was made of the effects of the constraints on the mechanisms of deformation and the patterns of distribution of strain wit作者: Pudendal-Nerve 時間: 2025-3-24 02:27
https://doi.org/10.1007/978-1-349-14240-8tation during myloni-tisation, intracrystalline rotation during plastic flow, and syntectonic recrystallisation. These model patterns are referred to principal directions of deviatoric stress, which cannot be reconstructed in many tectonites..Anhydrite tectonites are commonly pervaded by closely spa作者: bisphosphonate 時間: 2025-3-24 07:11
Globalization of Services: Friend or Foe?a is brittle up to about 200 bars confining pressure and failure occurs by extension and shear fractures. At higher confining pressures galena deforms by ductile faulting. Above 300 to 400 bars galena deforms be uniform flow and is ductile..The stress-strain curves show that the strength of galena i作者: 敲詐 時間: 2025-3-24 14:18
Global Carbon Dioxide Recyclingining pressure Sphalerite is brittle, above 1000 bar it is ductile. Strength of Sphalerite increases with increasing confining pressure. The results of derformation correspond with Mohr’s theory. The mechanical properties of Sphalerite are modified by accompanying material..By uni-axial deformation 作者: 膽小懦夫 時間: 2025-3-24 18:50
Global Cash Management in Europef any fabric) must contain a comparison of the spacial data and their degree of homogeneity as well as the symmetry features of various fabric elements .. This means that fabric investigation should not be limited to macroscopically visible features or to those observable only in the microscope. It 作者: Commonwealth 時間: 2025-3-24 20:10
Marc Lipsitch,Mauricio Santillanarmation and recry-stallization. Earlier work led to apparently conflicting results which are mostly resolved in this study. What emerges, however, is a complex picture of several different types of preferred orientation developed under different experimental conditions..In the .-quartz field, recrys作者: Assignment 時間: 2025-3-25 01:21
The Chickens Have Come Home to Roost, — 800°C, 5–10 kb confining pressure. At 800°C 10 kb, all single crystals oriented favorably for albite and pericline twin gliding have yield strengths of about 2 kb regardless of composition or structural state. Yield strengths of polycrystalline aggregates are 1.3 — 3.0 times greater. In both case作者: 含沙射影 時間: 2025-3-25 06:41
tural methods in connection with rock mechanic aspects. This area is situated at the northern border of the Norrland Geosyncline within the Swedish basement. Besides numerous field observations this work is to be referred to geology of the Renstr?m Mine (approximate depth 900 meters) and investigati作者: harbinger 時間: 2025-3-25 10:32 作者: Subdue 時間: 2025-3-25 13:57
diger (Dorfer-tal, Hohe Tauern, Eastalps). It was assumed that the steep B-axes was formed by compression parallel to the gentle regionally distributed B-axes. (Stauchfaltenbildung). The fabric is described as a syntectonic B ⊥ B’ type..The steep B-axes are dominant in the area of maximal compressio作者: AUGER 時間: 2025-3-25 17:05 作者: 舞蹈編排 時間: 2025-3-25 22:02
Global Business in Local Culturest commonly used is the Lambert Equal Area Projection (or Schmidt Net) and hence the accompanying computer listing pertains to this projection. However the programme is readily modified to construct other spherical projections.作者: 檢查 時間: 2025-3-26 00:27
A Computer Programme to Construct Spherical Projectionsst commonly used is the Lambert Equal Area Projection (or Schmidt Net) and hence the accompanying computer listing pertains to this projection. However the programme is readily modified to construct other spherical projections.作者: GROSS 時間: 2025-3-26 06:39 作者: 調(diào)整 時間: 2025-3-26 10:00 作者: Thyroxine 時間: 2025-3-26 15:33
The Use of X-Rays in Petrofabric Studiesle petrofabric technique, but there are inherent limitations. For a uniaxial mineral, such as quartz, only the attitude of the principal axis, and not the complete rotational attitude, can be determined unless there are visible morphological features such as cleavage or twinning. No results can be o作者: 注入 時間: 2025-3-26 20:08
Experimental Deformation of Constrained Crystals of Calcite in Extensionome evidence also for . glide..Two main effects of the constraint were evident. First, domains of heterogeneous deformation on the scale of the crystal, such as kinks, were no longer sharply defined, their boundaries being gradational in nature. Second, there was a tendency for glide to occur on mor作者: Charitable 時間: 2025-3-26 21:18 作者: adipose-tissue 時間: 2025-3-27 03:15 作者: Console 時間: 2025-3-27 05:50 作者: 厭倦嗎你 時間: 2025-3-27 09:49 作者: palette 時間: 2025-3-27 16:54
Der Schlingenbau im Grundgebirge des Renstr?mgebietes, Skelleftefeld, Nordschweden, in Montangeologire is classified with respect to the regional geology and local geological relations in point of view. The result of the investigations shows that in connection with the intrusion of later orogenic Revsund granite appears an isocline folding structure with steep overlaying axes of the mainly vertica作者: Emmenagogue 時間: 2025-3-27 20:00 作者: 治愈 時間: 2025-3-27 22:48 作者: exhilaration 時間: 2025-3-28 03:34
an indirect determination of data which have not been measured. In experimental structural petrology, the temperature and pressure dependence of the translational system has been studied in minerals from various types of rock formation which had not previously been investigated, and deductions were made conc978-3-642-95189-3978-3-642-95187-9作者: 盡忠 時間: 2025-3-28 06:45
https://doi.org/10.1007/978-981-99-9915-6le petrofabric technique, but there are inherent limitations. For a uniaxial mineral, such as quartz, only the attitude of the principal axis, and not the complete rotational attitude, can be determined unless there are visible morphological features such as cleavage or twinning. No results can be o作者: prostatitis 時間: 2025-3-28 13:06
Social Welfare and Competitivenessome evidence also for . glide..Two main effects of the constraint were evident. First, domains of heterogeneous deformation on the scale of the crystal, such as kinks, were no longer sharply defined, their boundaries being gradational in nature. Second, there was a tendency for glide to occur on mor作者: 清洗 時間: 2025-3-28 17:16
https://doi.org/10.1007/978-1-349-14240-8model for intragranular gliding possesses the main [010] maximum, but lacks girdles of [100] and [001]. Hence syntectonic recrystallization, probably accompanied by some intragranular rotation, seems to have been the main orienting mechanism. No speculations are warranted as to the role of annealing作者: Bronchial-Tubes 時間: 2025-3-28 21:35
Globalization of Services: Friend or Foe? be preserved during deformation and is superimposed by the axial symmetry of the new fabric. A theoretical derivation of the end position has been illustrated after the method of Taylor. The only result of the calculations was that [111] cannot be an end position..Comparison of the stress-strain cu作者: endocardium 時間: 2025-3-28 23:25
Marc Lipsitch,Mauricio Santillanarature and low strain-rate, orthorhombic strain due to temperature gradients produces “crossed girdles” of c-axes intersecting normal to σ.. An extended specimen shows c-axes concentrated at high angles to the extension direction, σ...In the ?-quartz field, recrystallization during compression yield作者: sperse 時間: 2025-3-29 03:25
The Chickens Have Come Home to Roost,ception, An.. 010 slip and concomitant kinking occur in the more sodic representatives, and irrational deformation lamellae occur in An.-An.. The latter are planar discontinuities in positions of high resolved shear stress and have strong preferred orientation with reference to the crystallographic 作者: STENT 時間: 2025-3-29 09:49 作者: intolerance 時間: 2025-3-29 13:06
Global Challenges for Identity Policiessively of quartz displaying different girdle patterns of extraordinarily high sharpness, using the A.V.A. technique, showed a clear correlation between the type of the orientation of the quartz, the symmetry in the distribution of the disclosed s-surfaces and the shapes of the quartz grains. A trial作者: farewell 時間: 2025-3-29 18:23
Conference proceedings 1970ay and experimental structural petrology. The Symposium of the Working Group on X-Ray and Experimental Structural Petrology, held at the invitation of the Deutsche Forschungsgemeinschaft on 17 and 18 February, 1969, in the Mineralogy Institute of the Technische Hochschule Darmstadt, was intended to 作者: 保全 時間: 2025-3-29 22:20 作者: 厭倦嗎你 時間: 2025-3-30 01:10
Global Cash Management in Europewas therefore a natural consequence that Sander, already in the early stages of petrofabric analysis, drew special attention to the possibilities of X-ray fabric analysis for the investigation of the smallest fabric units (Sander & Sachs 1930). These methods were later developed by Neff (1956), v. Gehlen (1960), Wenk (1965), and others.作者: 中子 時間: 2025-3-30 07:11
n and steep s-surfaces. In the adjoining northern areas with progressive minor compression and more gentle s-surface they loose their importance and eventually disappear. Then only the regional gentle B-axes are observed..This example shows the origin of a syntectonic steep B-axial fabric in regions with generally gentle B-axes.作者: precede 時間: 2025-3-30 09:49
Garnet Orientation in Different Metamorphic faciesby the preferred orientation of omphacite, quartz and calcite, too..The results partly agree with Kamb’s (1959) calculation for cubic minerals: [100] or [ 111 ] parallel to the main compression direction.作者: 他姓手中拿著 時間: 2025-3-30 13:58 作者: 移植 時間: 2025-3-30 19:26 作者: 柏樹 時間: 2025-3-30 23:37 作者: DEFER 時間: 2025-3-31 02:40 作者: 注入 時間: 2025-3-31 08:48
https://doi.org/10.1057/9781137412591e quartz-diagrams show a distinctive preferred orientation of poles of prism-planes a (1120) and m (lOlO), namely, am-girdle. At the part of the highest metamorphic grade the diagrams show almost nearly single one-crystal-fabrics through the positions of sub-planes of quartz. The mechanism of quartz-orientation was also discussed.作者: ADORN 時間: 2025-3-31 09:29
Global Business Value Innovationsmade by simply combining the appropriate anisotropy coefficients with area-corrected pole density data obtained from the contour values of [hk?]. distributions, and standard calculated intensities for the given material. Calculated and observed diffraction patterns for apatite in tibia of . and for calcite in Yule marble are in good agreement.作者: ABIDE 時間: 2025-3-31 13:45
https://doi.org/10.1007/978-3-658-11867-9n Polfigur. Sie liefert den Texturzustand von Proben in so kurzer Zeit, da? es damit m?glich ist, Untersuchungsprogramme auch gro?en Umfangs schnell abzuwickeln oder laufende Produktionskontrollen so schnell durchzuführen, da? man noch in den Fertigungsproze? eingreifen kann.作者: 意外的成功 時間: 2025-3-31 18:42 作者: landfill 時間: 2025-3-31 21:47
R?ntgenographische Gefügeanalyse [mit dem Z?hlrohr-Texturgoniometer] von Quarzschiefern aus Zentral-e quartz-diagrams show a distinctive preferred orientation of poles of prism-planes a (1120) and m (lOlO), namely, am-girdle. At the part of the highest metamorphic grade the diagrams show almost nearly single one-crystal-fabrics through the positions of sub-planes of quartz. The mechanism of quartz-orientation was also discussed.作者: 合唱團 時間: 2025-4-1 05:50 作者: 上流社會 時間: 2025-4-1 07:05 作者: acrophobia 時間: 2025-4-1 13:05 作者: Figate 時間: 2025-4-1 14:26
