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tectonic$81948$ - перевод на голландский
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![Plate motion based on [[Global Positioning System]] (GPS) satellite data from NASA [http://sideshow.jpl.nasa.gov/mbh/series.html JPL]. Each red dot is a measuring point and vectors show direction and magnitude of motion.](https://commons.wikimedia.org/wiki/Special:FilePath/Global plate motion 2008-04-17.jpg?width=200 "Plate motion based on [[Global Positioning System]] (GPS) satellite data from NASA [http://sideshow.jpl.nasa.gov/mbh/series.html JPL]. Each red dot is a measuring point and vectors show direction and magnitude of motion.")
![Global earthquake [[epicenter]]s, 1963–1998. Most earthquakes occur in narrow belts that correspond to the locations of lithospheric plate boundaries.](https://commons.wikimedia.org/wiki/Special:FilePath/Quake epicenters 1963-98.png?width=200 "Global earthquake [[epicenter]]s, 1963–1998. Most earthquakes occur in narrow belts that correspond to the locations of lithospheric plate boundaries.")
![1755 copper engraving depicting [[Lisbon]] in ruins and in flames after the [[1755 Lisbon earthquake]], which killed an estimated 60,000 people. A [[tsunami]] overwhelms the ships in the harbor.](https://commons.wikimedia.org/wiki/Special:FilePath/1755 Lisbon earthquake.jpg?width=200 "1755 copper engraving depicting [[Lisbon]] in ruins and in flames after the [[1755 Lisbon earthquake]], which killed an estimated 60,000 people. A [[tsunami]] overwhelms the ships in the harbor.")
![The tsunami of the [[2004 Indian Ocean earthquake]]](https://commons.wikimedia.org/wiki/Special:FilePath/2004-tsunami.jpg?width=200 "The tsunami of the [[2004 Indian Ocean earthquake]]")
![January 2017]] and the aftershocks (which continued to occur after the period shown here)](https://commons.wikimedia.org/wiki/Special:FilePath/2016 Central Italy earthquake wide.svg?width=200 "January 2017]] and the aftershocks (which continued to occur after the period shown here)")
![Messina earthquake]] and tsunami took almost 100,000 lives on December 28, 1908, in [[Sicily]] and [[Calabria]].<ref>"[http://news.bbc.co.uk/2/low/europe/2381585.stm Italy's earthquake history]." BBC News. October 31, 2002.</ref>](https://commons.wikimedia.org/wiki/Special:FilePath/Comerio, Luca (1878-1940) - Vittime del terremoto di Messina (dicembre 1908).jpg?width=200 "Messina earthquake]] and tsunami took almost 100,000 lives on December 28, 1908, in [[Sicily]] and [[Calabria]].<ref>\"[http://news.bbc.co.uk/2/low/europe/2381585.stm Italy's earthquake history].\" BBC News. October 31, 2002.</ref>")
![Reverse]]](https://commons.wikimedia.org/wiki/Special:FilePath/Fault types.svg?width=200 "Reverse]]")
![Ruins of the [[Għajn Ħadid Tower]], which collapsed during the [[1856 Heraklion earthquake]]](https://commons.wikimedia.org/wiki/Special:FilePath/Ghajn Hadid Tower closer view.JPG?width=200 "Ruins of the [[Għajn Ħadid Tower]], which collapsed during the [[1856 Heraklion earthquake]]")
![Haiti]], January 2010.](https://commons.wikimedia.org/wiki/Special:FilePath/Haiti earthquake damage.jpg?width=200 "Haiti]], January 2010.")
![Collapsed Gran Hotel building in the [[San Salvador]] metropolis, after the shallow [[1986 San Salvador earthquake]]](https://commons.wikimedia.org/wiki/Special:FilePath/HotelSanSalvador.jpg?width=200 "Collapsed Gran Hotel building in the [[San Salvador]] metropolis, after the shallow [[1986 San Salvador earthquake]]")
![Aerial photo of the San Andreas Fault in the [[Carrizo Plain]], northwest of Los Angeles](https://commons.wikimedia.org/wiki/Special:FilePath/Kluft-photo-Carrizo-Plain-Nov-2007-Img 0327.jpg?width=200 "Aerial photo of the San Andreas Fault in the [[Carrizo Plain]], northwest of Los Angeles")
![Fires of the [[1906 San Francisco earthquake]]](https://commons.wikimedia.org/wiki/Special:FilePath/Sfearthquake3b.jpg?width=200 "Fires of the [[1906 San Francisco earthquake]]")
Википедия
Tectonites are metamorphic or tectonically deformed rocks whose fabric reflects the history of their deformation, or rocks with fabric that clearly displays coordinated geometric features that indicate continuous solid (ductile) flow during formation. Planar foliation results from a parallel orientation of platey mineral phases such as the phyllosilicates or graphite. Slender prismatic crystals such as amphibole produce a lineation in which these prisms or columnar crystals become aligned. Tectonites are rocks with minerals that have been affected by natural forces of the earth, which allowed their orientations to change. This usually includes recrystallization of minerals, and the foliation formation. Tectonites are studied through structural analysis and allows for the determination of two things:
- The orientation of shearing and compressive stresses during (dynamic) metamorphism
- The later (or final) stages of metamorphism
According to the nature of mineral orientation, there are three main groups of tectonites, L-Tectonites, S-Tectonites, and LS-Tectonites. The different types reflect on the different ways that matter moves.
- L-Tectonites are aligned in a linear fabric, which allows the rock to split into rod-like shapes due to the two intersecting planes. The foliation of this type is not strong.
- S-Tectonites are the fabric that is dominantly a foliation fabric which allows the rock to split into plate-like sheets that are parallel to foliation. There are little to no linear fabrics within the foliation fabrics.
- LS-Tectonites is the perfect mix of the two, with both strong lineations and strong foliations. This is caused by the rotation of the grains around axes that are oriented along the trends of the folds.
