Cretaceous and Paleogene clinoform sequences of North Chukchi Basin

M.A. Agasheva; Y.A. Karpov; A.V. Stoupakova; A.A. Suslova

doi:10.3997/2214-4609.201701534

Cretaceous and Paleogene clinoform sequences of North Chukchi Basin
Authors M.A. Agasheva¹, Y.A. Karpov¹, A.V. Stoupakova¹, A.A. Suslova¹
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Affiliations: ¹ Lomonosov Moscow State University
Publisher: European Association of Geoscientists & Engineers
Source: Conference Proceedings, 79th EAGE Conference and Exhibition 2017, Jun 2017, Volume 2017, p.1 - 3
DOI: https://doi.org/10.3997/2214-4609.201701534

Abstract

Summary

A seismic and sequence stratigraphy framwork of the Cretaceous and Paleogene clinoform complexes are presented. The work is based on 2D regional seismic data and outcrop data.

The Cretaceos and Paleogene prograding clinoform successions infill the North Chukchi basin, formed during large-scale basin development in Early and Late Cretaceous.

The seismic analyis of clinoform defined that Cretaceous clinoform are represented mostly tangential oblique geometry. The Paleogene clinoform sequences characterized by various geometries - tangential oblique, sigmoidal and shingled types.

The Cretaceous and Paleogene clinoform sequences are mainly sourced from Wrangel-Herald Arch in the southern part of North Chukchi basin.

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2017-06-12

2024-04-24

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References

HouseknechtD.W., K.J.Bird and C.J.Schenk
, 2009, Seismic analysis of clinoform depositional sequences and shelf-margin trajectories in Lower Cretaceous (Albian) strata, Alaska North Slope: Basin Research, v. 21, p.644–654, doi: 10.1111/j.1365–2117.2008.00392.x.
https://doi.org/10.1111/j.1365–2117.2008.00392.x. [Google Scholar]
Hellan-Hansen, W., and Hampson, G.J.
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[Google Scholar]

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Cretaceous and Paleogene clinoform sequences of North Chukchi Basin

Conference Proceedings 2017, 1 (2017); https://doi.org/10.3997/2214-4609.201701534

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Abstract

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The natural combination of full and image‐based waveform inversion

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Characterizing the effect of elastic interactions on the effective elastic properties of porous, cracked rocks

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Laboratory measurements of guided‐wave propagation within a fluid‐saturated fracture