Reply to discussions by Zavala (2019) and by Van Loon, Hüeneke, and Mulder (2019) on Shanmugam, G. (2018, Journal of Palaeogeography, 7 (3): 197–238): ‘the hyperpycnite problem’
Abstract In this reply, I respond to 18 issues associated with comments made by Zavala (e.g., inverse- to normally-graded sequence, origin of massive sands, experimental sandy debris flows, tidal rhythmites, facies models, etc.), and 10 issues associated with comments made by Van Loon et al. (e.g.,...
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Online Access: | http://link.springer.com/article/10.1186/s42501-019-0047-1 |
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doaj-eb5a1f6e186a484abc0c385578f49d532020-11-25T04:08:09ZengSpringerOpenJournal of Palaeogeography2524-45072019-11-018111410.1186/s42501-019-0047-1Reply to discussions by Zavala (2019) and by Van Loon, Hüeneke, and Mulder (2019) on Shanmugam, G. (2018, Journal of Palaeogeography, 7 (3): 197–238): ‘the hyperpycnite problem’G. Shanmugam0Department of Earth and Environmental Sciences, The University of Texas at ArlingtonAbstract In this reply, I respond to 18 issues associated with comments made by Zavala (e.g., inverse- to normally-graded sequence, origin of massive sands, experimental sandy debris flows, tidal rhythmites, facies models, etc.), and 10 issues associated with comments made by Van Loon et al. (e.g., 16 types of hyperpycnal flows, anthropogenic hyperpycnal flow, etc.).http://link.springer.com/article/10.1186/s42501-019-0047-1Hyperpycnal flowsHyperpycnitesSandy debris flowsTurbidity currents |
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DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
G. Shanmugam |
spellingShingle |
G. Shanmugam Reply to discussions by Zavala (2019) and by Van Loon, Hüeneke, and Mulder (2019) on Shanmugam, G. (2018, Journal of Palaeogeography, 7 (3): 197–238): ‘the hyperpycnite problem’ Journal of Palaeogeography Hyperpycnal flows Hyperpycnites Sandy debris flows Turbidity currents |
author_facet |
G. Shanmugam |
author_sort |
G. Shanmugam |
title |
Reply to discussions by Zavala (2019) and by Van Loon, Hüeneke, and Mulder (2019) on Shanmugam, G. (2018, Journal of Palaeogeography, 7 (3): 197–238): ‘the hyperpycnite problem’ |
title_short |
Reply to discussions by Zavala (2019) and by Van Loon, Hüeneke, and Mulder (2019) on Shanmugam, G. (2018, Journal of Palaeogeography, 7 (3): 197–238): ‘the hyperpycnite problem’ |
title_full |
Reply to discussions by Zavala (2019) and by Van Loon, Hüeneke, and Mulder (2019) on Shanmugam, G. (2018, Journal of Palaeogeography, 7 (3): 197–238): ‘the hyperpycnite problem’ |
title_fullStr |
Reply to discussions by Zavala (2019) and by Van Loon, Hüeneke, and Mulder (2019) on Shanmugam, G. (2018, Journal of Palaeogeography, 7 (3): 197–238): ‘the hyperpycnite problem’ |
title_full_unstemmed |
Reply to discussions by Zavala (2019) and by Van Loon, Hüeneke, and Mulder (2019) on Shanmugam, G. (2018, Journal of Palaeogeography, 7 (3): 197–238): ‘the hyperpycnite problem’ |
title_sort |
reply to discussions by zavala (2019) and by van loon, hüeneke, and mulder (2019) on shanmugam, g. (2018, journal of palaeogeography, 7 (3): 197–238): ‘the hyperpycnite problem’ |
publisher |
SpringerOpen |
series |
Journal of Palaeogeography |
issn |
2524-4507 |
publishDate |
2019-11-01 |
description |
Abstract In this reply, I respond to 18 issues associated with comments made by Zavala (e.g., inverse- to normally-graded sequence, origin of massive sands, experimental sandy debris flows, tidal rhythmites, facies models, etc.), and 10 issues associated with comments made by Van Loon et al. (e.g., 16 types of hyperpycnal flows, anthropogenic hyperpycnal flow, etc.). |
topic |
Hyperpycnal flows Hyperpycnites Sandy debris flows Turbidity currents |
url |
http://link.springer.com/article/10.1186/s42501-019-0047-1 |
work_keys_str_mv |
AT gshanmugam replytodiscussionsbyzavala2019andbyvanloonhuenekeandmulder2019onshanmugamg2018journalofpalaeogeography73197238thehyperpycniteproblem |
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1724426593905934336 |