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Titlebook: Advances in Geomorphology and Quaternary Studies in Argentina; Proceedings of the S Jorge Rabassa Conference proceedings 2017 Springer Inte

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樓主: 富裕
21#
發(fā)表于 2025-3-25 04:31:54 | 只看該作者
https://doi.org/10.1057/9780230342927del Fuego under temperate/cold climate. The shape, size, perimeter and density of each pan are analysed, as well as the landforms developed in their periphery. The study was conducted in the San Sebastián Bay and between the Chico and Grande rivers, grouped according to the geomorphological unit in
22#
發(fā)表于 2025-3-25 10:01:41 | 只看該作者
23#
發(fā)表于 2025-3-25 12:41:52 | 只看該作者
Brett Pierce,Christabel Kalaiselvi of Jujuy, near the Argentine–Bolivian border. Geomorphologically, the area, which belongs to the Puna, has the distinctive characteristics of a bolson relief, covering an area of ~3650?km.. Puna is a large “altiplano,” a high-altitude tableland characteristic of the Central Andes. The depression sh
24#
發(fā)表于 2025-3-25 16:43:15 | 只看該作者
https://doi.org/10.1007/978-3-319-11722-5 and animals produce calcium biomineralizations, calcium oxalates and carbonates being the most representative. The Quaternary pedosedimentary sequences of the southeastern coast of Buenos Aires province evolved from bioclastic and loess sediments, reworked by water and/or wind action. Calcium biomi
25#
發(fā)表于 2025-3-25 22:10:02 | 只看該作者
26#
發(fā)表于 2025-3-26 03:09:02 | 只看該作者
Springer Earth System Scienceshttp://image.papertrans.cn/a/image/148130.jpg
27#
發(fā)表于 2025-3-26 06:24:23 | 只看該作者
28#
發(fā)表于 2025-3-26 10:49:11 | 只看該作者
978-3-319-85380-2Springer International Publishing AG 2017
29#
發(fā)表于 2025-3-26 15:40:24 | 只看該作者
Advances in Geomorphology and Quaternary Studies in Argentina978-3-319-54371-0Series ISSN 2197-9596 Series E-ISSN 2197-960X
30#
發(fā)表于 2025-3-26 18:20:57 | 只看該作者
https://doi.org/10.1057/9780230342927s peculiar landforms such as yardangs, mushrooms and hoodoos are observed. The dominant agents that are responsible for these features are chemical and physical weathering and aeolian erosion. The micro-modelling affecting the different ignimbrite units is a direct consequence of their particular te
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