Search Results - "Nexer, M."

"Arc-continent collision" of the Aleutian-Komandorsky arc into Kamchatka: Insight into Quaternary tectonic segmentation through Pleistocene marine terraces and morphometric analysis of fluvial drainage by Pedoja, K., Authemayou, C., Pinegina, T., Bourgeois, J., Nexer, M., Delcaillau, B., Regard, V.

“…At the NW corner of the Pacific region, just south of the Kamchatsky Peninsula, the northern tip of the Pacific plate subduction and associated volcanic arc…”
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Comment on “Active coastal thrusting and folding, and uplift rate of the Sahel Anticline and Zemmouri earthquake area (Tell Atlas, Algeria)”, by S. Maouche, M. Meghraoui, C. Morhange, S. Belabbes, Y. Bouhadad, H. Haddoum. [Tectonophysics, 2011, 509, 69–80] by Pedoja, K., Djellit, H., Authemayou, C., Deverchere, J., Strzerzynski, P., Heddar, A., Nexer, M., Boudiaf, A.

“…Based on geomorphologic analyses and leveling survey of Quaternary coastal indicators (i.e. marine terraces and notches) along of a 50-km-long coastal stretch…”
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Coastal staircase sequences reflecting sea-level oscillations and tectonic uplift during the Quaternary and Neogene by Pedoja, Kevin, Husson, Laurent, Johnson, Markes E., Melnick, Daniel, Witt, Cesar, Pochat, Stéphane, Nexer, Maëlle, Delcaillau, Bernard, Pinegina, Tatiana, Poprawski, Yohann, Authemayou, Christine, Elliot, Mary, Regard, Vincent, Garestier, Franck

“…Many coasts feature sequences of Quaternary and Neogene shorelines that are shaped by a combination of sea-level oscillations and tectonics. We compiled a…”
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Neogene-Quaternary slow coastal uplift of Western Europe through the perspective of sequences of strandlines from the Cotentin Peninsula (Normandy, France) by Pedoja, K., Jara-Muñoz, J., De Gelder, G., Robertson, J., Meschis, M., Fernandez-Blanco, D., Nexer, M., Poprawski, Y., Dugué, O., Delcaillau, B., Bessin, P., Benabdelouahed, M., Authemayou, C., Husson, L., Regard, V., Menier, D., Pinel, B.

“…The Cotentin Peninsula (Normandy, France) displays sequences of marine terraces and rasas, the latter being wide Late Cenozoic coastal erosion surfaces, that…”
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