Corps mince amoreiras

corps mince amoreiras

It primarily consists of syn-rift near-coastal continental siliciclastic sediments, with several marine intercalations.

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The primary flow direction was North to South, originating from Galicia and flowing between the Iberian landmass to the east and the now largely submerged Berlengas horsta North-South oriented ridgeto the west. Stratigraphy[ edit ] The unit was first formally proposed by Hill in Praia da Amoreira-Porto Novo Member[ edit ] The Praia da Amoreira-Porto Novo Member is composed of the Priaia de Amoreira Member, which consists of massive mudrock -sand with metre thick sandstone lenseswith massive mudrock with calcrete.

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The overlying Poto Novo Mb. The environment of deposition is interpreted as a meandering fluvial system, while the Porto Novo Mb is interpreted as a deltaic deposit. It is interpreted to be latest Kimmeridgian in age. South of Santa Cruz primarily consists of sandstone with rare conglomerate.

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The age is considered to corps mince amoreiras latest Kimmeridigan to earliest Tithonian. Assenta Member[ edit ] The Assenta Member is around metres thick and predominantly consists of mudstones with frequent layers of caliche.

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Near the top of the member several layers of tens of metres thick nodular and marly bioclastic limestones are present, containing marine benthic foramsthe nodularity is derived from intense Thalassinoides burrowing. It is predominately late Tithonian in age, with the last few metres probably being earliest Berriasian.

Crâne exposé au muséum d'histoire naturelle d'Oklahoma. Le paléontologue Gregory S. Ces dents longues, aplaties et crantées dentition zyphodonte devenaient plus courtes, plus étroites et plus courbées vers le fond de la gueule. Comme elles tombaient facilement et étaient remplacées en permanence, ce sont de nos jours des fossiles communs [3]. Le crâne, très léger, était fait essentiellement de barres osseuses séparées par de grands vides.

The environment of deposition is interpreted as being an upper fluvial-dominated delta to meandering fluvial systems flowing on a paralic plain.

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