Titlebook: Gondwana Landscapes in southern South America; Argentina, Uruguay a Jorge Rabassa,Cliff Ollier Book 2014 Springer Science+Business Media Do

使迷醉

土坯

深陷

Ancient Landscapes of Uruguay,ural framework of the landscape evolution is provided and the record of such evolution in the most representative geological units is considered. A brief summary of the Uruguayan geology and its location in the regional context is performed, from Precambrian to Cenozoic times..From the analysis of t

nitroglycerin

A General Overview of Gondwana Landscapes in Argentina,her geologists and naturalists of the different European schools that worked in this country. These studies were continued at a very good level in Brazil, thanks to the work of Lester C. King, later on intensively followed by Jo?o José Bigarella. However, these concepts gradually disappeared from th

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anaphylaxis

Geomorphology of Paleosurfaces in the Sierras de Comechingones, Central Pampean Ranges, Argentina,ampeanas of Argentina. Their origin and age are still under discussion, but in general, it is assumed that they correspond to etchplains and pediplains developed between the Middle-Late Jurassic and the Paleogene. The objective of this chapter is to present a morphological-morphometric characterizat

concubine

Gondwana Glacial Paleolandscape, Diamictite Record of Carboniferous Valley Glaciation, and Preglacinzo basin. Previous investigations have focused on the sandstones in the paleovalley and inferred a glacial lacustrine history. New observations have demonstrated that remnants of a preglacial, ancient weathering front, developed under wet tropical conditions and composed of corestones, are found un

inventory

Planation Surfaces of Central Western Argentina,l, tectonic, and geomorphological domains. Preserved remnants of planation surfaces, which form the summit of major geological units, occur as discontinuous and isolated exposures with a remarkable geographical distribution along 600 km (33°–39° S). The main goal of this chapter is to summarize the

frozen-shoulder

Erosion Surface and Granitic Morphology in the Sierra de Lihuel Calel, Province of La Pampa, Argentrom SRTM were used for the analysis of morphometric characteristics and other parameters, so as to obtain longitudinal profiles and identify the boundaries of the paleosurface. By means of the interpretation of satellite imagery and field observations, the different features of this ancient landscap

Heterodoxy

Paleo-landscapes of the Northern Patagonian Massif, Argentina, (plutonic and metamorphic rocks), eruptive rocks of the Gondwana cycle (Early to Middle Carboniferous), and Jurassic volcanic rocks..The most important active climate during the genesis of this surface had a very significant role, developing intense chemical weathering extending to variable depths