Review of research in internal-wave and internal-tide deposits of China: Discussion

This discussion of a review article by [27], published in the Journal of Palaeogeography (2(1): 56– 65), is aimed at illustrating that interpretations of ten ancient examples in China and one in the central Appalachians (USA) as deep-water deposits of internal waves and internal tides are unsustaina...

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Main Author: G. Shanmugam
Format: Article
Language:English
Published: SpringerOpen 2014-10-01
Series:Journal of Palaeogeography
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2095383615300894
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spelling doaj-3c5f1eb71f2840abb727f7eaea9e36b12020-11-25T01:54:27ZengSpringerOpenJournal of Palaeogeography2095-38362014-10-013433235010.3724/SP.J.1261.2014.00060Review of research in internal-wave and internal-tide deposits of China: DiscussionG. ShanmugamThis discussion of a review article by [27], published in the Journal of Palaeogeography (2(1): 56– 65), is aimed at illustrating that interpretations of ten ancient examples in China and one in the central Appalachians (USA) as deep-water deposits of internal waves and internal tides are unsustainable. This critical assessment is based on an in-depth evaluation of oceanographic and sedimentologic data on internal waves and internal tides derived from 332 print and online published works during 1838–January 2013, which include empirical data on the physical characteristics of modern internal waves and internal tides from 51 regions of the world’s oceans [108]. In addition, core and outcrop descriptions of deep-water strata from 35 case studies worldwide carried out by the author during 1974–2011, and a selected number of case studies published by other researchers are evaluated for identifying the sedimentological challenges associated with distinguishing types of bottom-current reworked sands in the ancient sedimentary record. The emerging conclusion is that any interpretation of ancient strata as deposits of internal waves and internal tides is premature.http://www.sciencedirect.com/science/article/pii/S2095383615300894baroclinic sandscontour currentsdeep waterfacies modelsinternal wavesinternal tidespycnoclinesshelf edge
collection DOAJ
language English
format Article
sources DOAJ
author G. Shanmugam
spellingShingle G. Shanmugam
Review of research in internal-wave and internal-tide deposits of China: Discussion
Journal of Palaeogeography
baroclinic sands
contour currents
deep water
facies models
internal waves
internal tides
pycnoclines
shelf edge
author_facet G. Shanmugam
author_sort G. Shanmugam
title Review of research in internal-wave and internal-tide deposits of China: Discussion
title_short Review of research in internal-wave and internal-tide deposits of China: Discussion
title_full Review of research in internal-wave and internal-tide deposits of China: Discussion
title_fullStr Review of research in internal-wave and internal-tide deposits of China: Discussion
title_full_unstemmed Review of research in internal-wave and internal-tide deposits of China: Discussion
title_sort review of research in internal-wave and internal-tide deposits of china: discussion
publisher SpringerOpen
series Journal of Palaeogeography
issn 2095-3836
publishDate 2014-10-01
description This discussion of a review article by [27], published in the Journal of Palaeogeography (2(1): 56– 65), is aimed at illustrating that interpretations of ten ancient examples in China and one in the central Appalachians (USA) as deep-water deposits of internal waves and internal tides are unsustainable. This critical assessment is based on an in-depth evaluation of oceanographic and sedimentologic data on internal waves and internal tides derived from 332 print and online published works during 1838–January 2013, which include empirical data on the physical characteristics of modern internal waves and internal tides from 51 regions of the world’s oceans [108]. In addition, core and outcrop descriptions of deep-water strata from 35 case studies worldwide carried out by the author during 1974–2011, and a selected number of case studies published by other researchers are evaluated for identifying the sedimentological challenges associated with distinguishing types of bottom-current reworked sands in the ancient sedimentary record. The emerging conclusion is that any interpretation of ancient strata as deposits of internal waves and internal tides is premature.
topic baroclinic sands
contour currents
deep water
facies models
internal waves
internal tides
pycnoclines
shelf edge
url http://www.sciencedirect.com/science/article/pii/S2095383615300894
work_keys_str_mv AT gshanmugam reviewofresearchininternalwaveandinternaltidedepositsofchinadiscussion
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