File:Cataclasita.png
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Captions
Captions
Distribution of the main types of fault rocks in the depth of the crust.
Summary edit
| Description |
Español: Distribución de los principales tipos de rocas de falla en la profundidad de la corteza. A) Diagrama esquemático de cuatro rocas de falla típica (sin escala) y la geometría local de la zona de corte en un bloque de 1 m de ancho, tal como se desarrollaría a partir de un granito de fenocristalino. Las zonas de corte inclinadas (normales o inversas) muestran una distribución similar de rocas de falla y geometría de la zona de corte en la profundidad de la corteza. B) Sección transversal esquemática a través de una zona de cizallamiento transcurrente. La zona puede ensancharse y se producen cambios en la geometría y el tipo dominante de roca de falla al aumentar la profundidad y el grado metamórfico. Esta imagen esta basado en la pagina Web de Alex Strekeisen, Cataclasite
English: Distribution of the main types of fault rocks in the depth of the crust. A) Schematic diagram of four typical fault rocks (without scale) and the local geometry of the cut zone in a 1 m wide block, as it would be developed from a granite of phenocrystals. The inclined cut zones (normal or inverse) show a similar distribution of fault rocks and geometry of the cut zone in the depth of the crust. B) Schematic cross section through a zone of transverse shear. The area can widen and changes in the geometry and dominant type of fault rock occur with increasing depth and metamorphic grade. This image is based on Alex Strekeisen's website, Cataclasite |
| Date | |
| Source | Own work |
| Author | Chiche Ojeda |
| Camera location |  | View this and other nearby images on: OpenStreetMap |  |
|---|
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File history
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 18:35, 11 May 2020 | | 1,307 × 754 (280 KB) | Chiche Ojeda (talk | contribs) | 1. En el esquema de los gneises bandeados las bandas eran paralelas, ahora se cambió adptandose a los blastos. La foliación en los gneises glandulares se adapta a los blastos de feldespato, los rodea. Los blastos se estiraron en la dirección de la deformación de cizalla dúctil hasta dar una forma de bandas. 2. Se retiró la firma del autor:Chiche Ojeda 3. Se cambiaron los siguientes textos: - granito fenocristal por granito fenocristalino. - roca frágil con cataclasita cohesiva por falla fr... |
| 18:06, 27 April 2020 |  | 1,346 × 792 (254 KB) | Chiche Ojeda (talk | contribs) | Se cambio la palabra mielonita por la palabra milonita y se le puso un marco alrededor de toso el gráfico. | |
| 02:14, 18 April 2020 |  | 1,307 × 756 (255 KB) | Chiche Ojeda (talk | contribs) | Uploaded own work with UploadWizard |
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