Zobrazeno 1 - 10
of 87
pro vyhledávání: '"Cyclic sedimentation"'
Autor:
Veronica Rossi, Alessandro Amorosi, Giulia Barbieri, Stefano Claudio Vaiani, Matteo Germano, Bruno Campo
Publikováno v:
Geosciences, Vol 11, Iss 10, p 401 (2021)
Understanding Quaternary dynamics of delta-coastal plains across multiple glacial-interglacial cycles in the Milankovitch band (~100 kyrs) is crucial to achieve a robust evaluation of possible environmental response to future climate-change scenarios
Externí odkaz:
https://doaj.org/article/4ebf1c7b44d2481b8360a6393f38f9ed
Publikováno v:
Tanzania Journal of Science; Vol. 47 No. 5 (2021); 1530-1545
This research focused on the interpretation of paleodepositional environment and development of a sequence stratigraphic framework for the well TN-1 section, located in the coastal swamp depositional belt of the Niger Delta Basin. Integration of inte
Publikováno v:
Geologos, Vol 21, Iss 4, Pp 285-302 (2015)
Markov chain analysis was applied to studies of cyclic sedimentation in the Coal Complex of the Bełchatów mining field (part of the Bełchatów lignite deposit). The majority of ambiguous results of statistical testing that were caused by weak, sta
Externí odkaz:
https://doaj.org/article/2793341b6bd44de7a597eae57a716e6c
Autor:
EDUARDO GARZANTI, MARCO PAGNI FRETTE
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 96, Iss 4 (2017)
The Carnian sedimentary succession of the Lierna area, more than 4OO m thick and belonging to the Coltignone tectonic unit (Grigne Group), has considerable paleogeographic significance, for it documents the western termination of the deltalagoon-carb
Externí odkaz:
https://doaj.org/article/cbe4d3a55fa74ff7aef496c5ee235dcb
Autor:
Luis A Spalletti, Ana María Zavattieri
Publikováno v:
Andean Geology, Vol 36, Iss 2, Pp 236-263 (2009)
El depocentro triásico de Santa Clara, Cuenca Cuyana, se caracteriza por espesos depósitos generados en ambiente lacustre. Uno de ellos, con un registro de más de 345 m, corresponde a la Formación Mollar. El tramo inferior a medio está caracteri
Externí odkaz:
https://doaj.org/article/320f5e225e0749d0a0bd537591ead410
Autor:
Alessandro Amorosi, Bruno Campo, Matteo Germano, Giulia Barbieri, Veronica Rossi, Stefano Claudio Vaiani
Publikováno v:
Geosciences, Vol 11, Iss 401, p 401 (2021)
Geosciences
Volume 11
Issue 10
Geosciences
Volume 11
Issue 10
Understanding Quaternary dynamics of delta-coastal plains across multiple glacial-interglacial cycles in the Milankovitch band (~100 kyrs) is crucial to achieve a robust evaluation of possible environmental response to future climate-change scenarios
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Publikováno v:
Gilbert, G L, Cable, S, Thiel, C, Christiansen, H H & Elberling, B 2017, ' Cryostratigraphy, sedimentology, and the late Quaternary evolution of the Zackenberg River delta, northeast Greenland ', Cryosphere, vol. 11, no. 3, pp. 1265-1282 . https://doi.org/10.5194/tc-11-1265-2017
The Cryosphere, Vol 11, Pp 1265-1282 (2017)
The Cryosphere
The Cryosphere, Vol 11, Pp 1265-1282 (2017)
The Cryosphere
The Zackenberg River delta is located in northeast Greenland (74°30′ N, 20°30′ E) at the outlet of the Zackenberg fjord valley. The fjord-valley fill consists of a series of terraced deltaic deposits (ca. 2 km2) formed during relative sea-level
Publikováno v:
Geologos, Vol 21, Iss 4, Pp 285-302 (2015)
Markov chain analysis was applied to studies of cyclic sedimentation in the Coal Complex of the Bełchatów mining field (part of the Bełchatów lignite deposit). The majority of ambiguous results of statistical testing that were caused by weak, sta
Autor:
GARZANTI, EDUARDO, PAGNI FRETTE, MARCO
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 96, Iss 4 (2017)
Rivista Italiana di Paleontologia e Stratigrafia (Research In Paleontology and Stratigraphy); V. 96, N. 4
Rivista italiana di Paleontologia e Stratigrafia; V. 96, N. 4
Rivista Italiana di Paleontologia e Stratigrafia (Research In Paleontology and Stratigraphy); V. 96, N. 4
Rivista italiana di Paleontologia e Stratigrafia; V. 96, N. 4
The Carnian sedimentary succession of the Lierna area, more than 4OO m thick and belonging to the Coltignone tectonic unit (Grigne Group), has considerable paleogeographic significance, for it documents the western termination of the deltalagoon-carb