نتایج جستجو برای: ichnofacies

تعداد نتایج: 46  

Journal: :Spanish journal of palaeontology 2021

Relatively diverse trace fossils made by insects, other arthropods and oligochaete worms occur in the Miocene lacustrine marginal deposits of Calatayud-Teruel basin (NE Spain). They include ichnospecies Celliforma isp., Celliforma? isp. A B, aff. habari, Rosellichnus cf. arabicus, Spongeliomorpha Labyrintichnus terrerensis n. igen. et Taenidium barreti, Beaconites filiformis Polykladichnus arag...

Journal: :Sains Malaysiana 2021

There have been many disagreements regarding the depositional environment of Oligocene Tajau Sandstone Member Kudat Formation, Northern Sabah. We present here, first detailed sedimentary facies analysis for Member, exposed on Peninsula. The identified are interpreted as deposits subaqueous sediment density flows, which common processes in deep marine settings. These include debrites, hyperconce...

Journal: :journal of sciences, islamic republic of iran 2011
n abbassi

the kashkan formation (paleocene to middle eocene), consists of conglomerate, sandstone, and siltstone in the zagros folded zone, southwest iran. type of the sedimentary facies, architectural elements and trace fossils show that kashkan deposits were formed in a low sinuosity braided stream system, with north to south flow direction. the formation displays coarsening-upward succession reflects ...

2016
Jennifer F. Parker Philip J. Hopley Brian F. Kuhn

The Buxton-Norlim Limeworks southwest of Taung, South Africa, is renowned for the discovery of the first Australopithecus africanus fossil, the 'Taung Child'. The hominin was recovered from a distinctive pink calcrete that contains an abundance of invertebrate ichnofauna belonging to the Coprinisphaera ichnofacies. Here we describe the first fossil bee's nest, attributed to the ichnogenus Celli...

N Abbassi

The Kashkan Formation (Paleocene to Middle Eocene), consists of conglomerate, sandstone, and siltstone in the Zagros Folded zone, southwest Iran. Type of the sedimentary facies, architectural elements and trace fossils show that Kashkan deposits were formed in a low sinuosity braided stream system, with north to south flow direction. The formation displays coarsening-upward succession reflects ...

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