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書目名稱Geomorphology of the Northeast Region of Brazil影響因子(影響力)




書目名稱Geomorphology of the Northeast Region of Brazil影響因子(影響力)學科排名




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書目名稱Geomorphology of the Northeast Region of Brazil網(wǎng)絡公開度學科排名




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書目名稱Geomorphology of the Northeast Region of Brazil讀者反饋學科排名

Bereavement

Geomorphology of Paraíba Statete landform compartments, including the Borborema Highlands and the Sertaneja lowlands, are dominated by the drier climatic conditions associated with the semi-arid domain, with year-round high temperatures and precipitation averaging 400–800?mm. This scenario is associated with thinner soils covere

Mercurial

Picks-Disease

Geomorphology of Alagoas Stateresidual landforms of Santana, Mata Grande, and água Branca massifs, the fluvial and coastal plains, and the escarpments of the Borborema Highlands have also been identified as morphostructural sub-units. A new subdivision of the State’s macro-relief units was proposed based on the relationship betw

暴露他抗議

Geomorphology of Sergipe Statee rocks. About landscapes of large rivers, there is evidence of neotectonic activity, exhibited by the Canyons of the S?o Francisco, Vaza Barris and also the Submarine Canyon of the mouth of the Japaratuba River. The coastal tablelands are found in several stretches under heavy dissection, when inte

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Geomorphology of Bahia Stateiences. We highlight that these two fundamental works and other studies are extensive, sometimes difficult to understand, and inaccessible to the majority of the public. Therefore, a careful and synthetic geomorphological discussion is outlined. The reflections produced in this scientific work confi

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狼群

Kreisprozesse und Energiewandlung,te landform compartments, including the Borborema Highlands and the Sertaneja lowlands, are dominated by the drier climatic conditions associated with the semi-arid domain, with year-round high temperatures and precipitation averaging 400–800?mm. This scenario is associated with thinner soils covere

褻瀆

https://doi.org/10.1007/978-3-319-93852-3e and the inland semi-arid, corresponding to continuous or fragmented alluvial plains and terraces according to the discharge regime, that varies from perennial to ephemeral. Overall, the morphological units are distributed as a succession of “stepped” surfaces starting from the coast, increasing in

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