| dbo:abstract |
في الجيولوجيا، يحدث التداخل أو التعاقب عندما تقع أديمات (طبقات أو صخور) من ليثولوجيا معينة بين أديمات من ليثولوجيا مختلفة. على سبيل المثال، قد تكون الصخور الرسوبية متداخلة إذا كانت هناك اختلافات في مستوى سطح البحر في بيئتها الرسوبية. (ar) Unter Wechsellagerung wird in der Geologie eine Schichtung verstanden, in der abwechselnd Schichten (meist von Sedimentgesteinen) mit deutlich unterschiedlichen petrographischen Eigenschaften (Lithologien), beispielsweise einer deutlich unterschiedlichen chemischen Zusammensetzung, aufeinanderfolgen. Eine derartig aufgebaute Schichtenfolge wird als Wechselfolge bezeichnet. Bei Abfolgen, in denen sich lediglich zwei verschiedene Lithologien abwechseln, spricht man auch von alternierendem Schichtwechsel. (de) In geology, interbedding occurs when beds (layers of rock) of a particular lithology lie between or alternate with beds of a different lithology. For example, sedimentary rocks may be interbedded if there were sea level variations in their sedimentary depositional environment. Intercalation is a special case of interbedding where a layer is variably inserted into an already existing sequence; or where two separate depositional environments in close spatial proximity migrate alternately across the contact. While interbedding has layers that are horizontally flat (or aligned with the angle of the entire stratum), intercalated rock on the other hand has slanted layers that streak through each other (even when it aligns with the stratum). For example intercalated conglomerate and sandstone looks like ripples of different material networked through each other somewhat off the horizontal, as the beds are deposited in a gradient. This is likely due to differing fluvial conditions and gradual changes in sediment transport over time. (en) |
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في الجيولوجيا، يحدث التداخل أو التعاقب عندما تقع أديمات (طبقات أو صخور) من ليثولوجيا معينة بين أديمات من ليثولوجيا مختلفة. على سبيل المثال، قد تكون الصخور الرسوبية متداخلة إذا كانت هناك اختلافات في مستوى سطح البحر في بيئتها الرسوبية. (ar) Unter Wechsellagerung wird in der Geologie eine Schichtung verstanden, in der abwechselnd Schichten (meist von Sedimentgesteinen) mit deutlich unterschiedlichen petrographischen Eigenschaften (Lithologien), beispielsweise einer deutlich unterschiedlichen chemischen Zusammensetzung, aufeinanderfolgen. Eine derartig aufgebaute Schichtenfolge wird als Wechselfolge bezeichnet. Bei Abfolgen, in denen sich lediglich zwei verschiedene Lithologien abwechseln, spricht man auch von alternierendem Schichtwechsel. (de) In geology, interbedding occurs when beds (layers of rock) of a particular lithology lie between or alternate with beds of a different lithology. For example, sedimentary rocks may be interbedded if there were sea level variations in their sedimentary depositional environment. Intercalation is a special case of interbedding where a layer is variably inserted into an already existing sequence; or where two separate depositional environments in close spatial proximity migrate alternately across the contact. (en) |
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تداخل (جيولوجيا) (ar) Wechsellagerung (de) Interbedding (en) |
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