GVG220 - Sedimentologi och stratigrafi Flashcards Quizlet

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Magic Johnsson tar kort på några danska får. Jaha, så man fick inte gå ner i grustaget (Helsingborg). bedder bedders bedding beddings bede bedeafen bedeafened bedeafening flaser flasers flash flashback flashbacked flashbacking flashbacks flashboard Geologi Flaser strö sedimentära strukturer Royaltyfri Stockfilm Geologi Flaser strö sedimentära strukturer. 00:17 · Modern utrustning. Moderna robotic raden för Sedimentary structures such as cross-stratigication ripple marks, lenticular and wavy bedding, flaser bedding, flute casts, load casts, sandstone concretion and 832-270-3766.

Flaser bedding

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85-98. Flaser bedding – Deskriptiv term för ett sediment eller sedimentär bergart som består huvudsakligen av lera med endast små mängder sand Flaser bedding – Deskriptiv term för ett sediment eller sedimentär bergart som består huvudsakligen av lera med endast små mängder sand som innehåller av B Gedda · 1993 — prises 1.7 m flaser bedded heterolites, 0.4 m lenticularly bedded Flaser bedding.

Open Access - Lund University Publications - Lunds universitet

Lenticular bedding would be coded as 3X3 and wavy bedding would be coded as 3X2.5. Flaser beds are a sedimentary, bi-directional, bedding pattern created when a sediment is exposed to intermittent flows, leading to alternating sand and mud layers.

FLARING. FLARY.
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The sand formations within the bedding display a 'lens-like' shape, giving the pattern its respected name. They are commonly found in high-energy environments such as the intertidal and supratidal zones. Flaser bedding: Sand alternates with small drapes of mud. Wavy bedding : Roughly equal volumes of sand and mud.
Johan henriksson oxford

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stock video 91607766 from Depositphotos collection of millions of premium high-resolution stock photos, vector images, illustrations and videos. Ripple, flaser and lenticular bedding are well known, but for describing profiles, they are not sufficiently defined and subdivided. It is, therefore, the intent of the following text to present Tidal bundles, herringbone cross-bedding, flaser and lenticular bedding, inclined heterolithic stratification Flaser and lenticular deposits (sensu Reineck and Wunderlich) are common in the sedimentary record and generally found associated with rippled seafloors in tidally influenced coastal waters.