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Miquel Poyatos-Moré

Researcher at University of Oslo

Publications -  46
Citations -  439

Miquel Poyatos-Moré is an academic researcher from University of Oslo. The author has contributed to research in topics: Sedimentary depositional environment & Sedimentary rock. The author has an hindex of 10, co-authored 31 publications receiving 291 citations. Previous affiliations of Miquel Poyatos-Moré include University of Manchester & University of Leeds.

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Transport and deposition of mud in deep‐water environments: Processes and stratigraphic implications

TL;DR: In this article, the authors present a dataset from a 538.50 m-thick cored succession through the Permian muddy lower Ecca Group of the Tanqua depocentre (southwest Karoo Basin, South Africa).
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Mud-Dominated Basin-Margin Progradation: Processes and Implications

TL;DR: In this paper, the authors study the role of fine-grained sediment in basin-margin progradation in the absence of sand supply, and demonstrate how the accretion of fine grained sediment can play a significant role in basin margin prediction.
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Topographic controls on the development of contemporaneous but contrasting basin-floor depositional architectures

TL;DR: In this article, an analysis of depositional architecture and stacking patterns along a 70 km dip-oriented transect in the Upper Broto Turbidite System (Jaca Basin, south-central Pyrenees, Spain), which displays disparate stacking patterns in contemporaneous strata is presented.
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Filter Or Conveyor? Establishing Relationships Between Clinoform Rollover Trajectory, Sedimentary Process Regime, and Grain Character Within Intrashelf Clinothems, Offshore New Jersey, U.S.A.

TL;DR: In this article, an integrated study of clinoform rollover trajectory and detailed grain character analysis is presented to assess the role of top-set process regime in determining sand distribution and sediment character across clinothems.
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Disconnected submarine lobes as a record of stepped slope evolution over multiple sea-level cycles

TL;DR: In this article, the effects of abrupt changes in slope angle and orientation on turbidity current behavior have been investigated in numerous physical and numerical experiments and examined in outcrop, subsurface, and modern systems.