Mechanisms of late Quaternary fault throw-rate variability along the north central Gulf of Mexico coast: implications for coastal subsidence-Reference-Cited by-同舟云学术

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Mechanisms of late Quaternary fault throw-rate variability along the north central Gulf of Mexico coast: implications for coastal subsidence

Published:2016-02-23 Issue:5 Volume:29 Page:557-570
ISSN:0950-091X
Container-title:Basin Research
language:en
Short-container-title:Basin Res

Author:

Shen Zhixiong¹²^ORCID,Dawers Nancye H.²,Törnqvist Torbjörn E.²,Gasparini Nicole M.²,Hijma Marc P.²³,Mauz Barbara⁴

Affiliation:

1. Department of Marine Science; Coastal Carolina University; Conway SC USA

2. Department of Earth and Environmental Sciences; Tulane University; New Orleans LA USA

3. Department of Applied Geology and Geophysics; Deltares; Utrecht The Netherlands

4. School of Environmental Sciences; University of Liverpool; Liverpool UK

Funder

Gulf Coast Association of Geological Societies award

Tulane/Xavier Center for Bioenvironmental Research

Publisher

Wiley

Subject

Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/bre.12184/fullpdf

Reference79 articles.

1. Dose-rate conversion factors: update;Adamiec;Ancient TL,1998

2. Controls on turbidite sand deposition during gravity-driven extension of a passive margin: examples from miocene sediments in block 4, Angola;Anderson;Mar. Pet. Geol.,2000

3. Influence of growth faults on coastal fluvial systems: examples from the late miocene to recent Mississippi River delta;Armstrong;Sed. Geol.,2014

4. Causes of river avulsion: insights from the late holocene avulsion history of the Mississippi River, U.S.A;Aslan;J. Sediment. Res.,2005

5. Stratigraphic development of synkinematic deposits in a large growth-fault system, onshore brunei darussalam;Back;J. Geol. Soc.,2005

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