Zobrazeno 1 - 10
of 239
pro vyhledávání: '"Flandrian interglacial"'
Autor:
Boyd, W. E., Dickson, J. H.
Publikováno v:
The New Phytologist, 1987 Sep 01. 107(1), 221-244.
Externí odkaz:
https://www.jstor.org/stable/2434893
Publikováno v:
Известия высших учебных заведений: Геология и разведка, Vol 0, Iss 6, Pp 59-65 (2019)
The results of studying and assessment of the impact of climate change on the groundwater in the Mekong delta have indicated that the exploitation of quaternary aquifers is not enough to solve the task of water supply in the region. Therefore, in the
Autor:
A. Min, C. R. Shadik, R. L. Edwards, Mark B. Bush, G. M. Cárdenes-Sandí, Alexander Correa-Metrio
Publikováno v:
Journal of Paleolimnology. 58:497-510
The last interglacial was the most recent time when temperatures were 1–2 °C above modern, but little is known of this period in the lowland Neotropics. Equally, data for the full glacial period are very limited. A detailed analysis of the period
Autor:
A. M. Celâl Şengör, Tayfun Kindap
Publikováno v:
World Geomorphological Landscapes ISBN: 9783030035136
The city of Istanbul is one of the most ancient sites of human dwelling in the world that has been continuously inhabited until today. It may indeed be the oldest. It enjoys a temperate climate characterised by wet winters and dry summers, although s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::54308cbde494a4024f0dc2244279c628
https://doi.org/10.1007/978-3-030-03515-0_10
https://doi.org/10.1007/978-3-030-03515-0_10
Autor:
Anthony Kirkham, Graham Evans
Publikováno v:
Sabkha Ecosystems ISBN: 9783030044169
The Flandrian transgression inundated an embayed Abu Dhabi coastline defined by headlands dominated by Miocene and Quaternary continental strata. Subsequent coastal development has produced the sabkha where Holocene marine carbonate dominates the out
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::debf7c5e2707abb82d34cb24a8b8f58e
https://doi.org/10.1007/978-3-030-04417-6_3
https://doi.org/10.1007/978-3-030-04417-6_3
Autor:
V. A. Dergachev
Publikováno v:
Geomagnetism and Aeronomy. 56:908-913
This paper analyzes climate changes since the end of the last glaciations 19–20 thousand years ago, including the modern warm interglacial Holocene age, which started about 11.5 thousand years ago. The connection between the impact of the orbital e
Autor:
Mohammadreza Gharibreza
Publikováno v:
Quaternary International. 392:203-212
The Coastal Makrn (CM) is the outermost part of the Makran zone, which is one of few intact areas to study the evolutionary trend of raised beaches and also to estimate the rate of coastal progradation since the late Holocene. The Makran zone is an a
Autor:
Prasanta Kumar Sen, Manju Banerjee
Publikováno v:
International Journal of Geosciences. :615-629
Biostratigraphic Zones Bb. Bz. H. I-V distinguished in C14 dated Peat, peaty clay sediments above arid, Barren zone have identified distinct environment of deposition as fresh water mixed brackish water to shallow marine to brackish water mangrove sw
Autor:
Daniel Barragán Mallofret
Publikováno v:
Revista Atlántica-Mediterránea de Prehistoria y ArqueologÃa Social. 18:111-138
This work presents a brief sinthesis of the theoretical starting points and the investigative results of the doctoral dissertation The Flandrian Transgression in the alluvial plain near Sevilla. The Guadalquivir river palaeoestuary, which includes th
Publikováno v:
The Spanish Coastal Systems ISBN: 9783319931685
The estuary of the Odiel and Tinto rivers is located in the southwest of the Iberian Peninsula on the western Gulf of Cadiz (Atlantic Ocean). The Huelva estuary is constituted by the common mouth of the Odiel and Tinto Rivers in a “Y” shape orien
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3e003253ffbe2c27fd24c5f1c9e4e52e
https://doi.org/10.1007/978-3-319-93169-2_23
https://doi.org/10.1007/978-3-319-93169-2_23