LEADER 03514nam 22006255 450 001 9910299434103321 005 20200701064610.0 010 $a3-319-18203-X 024 7 $a10.1007/978-3-319-18203-2 035 $a(CKB)3710000000416821 035 $a(EBL)2095726 035 $a(SSID)ssj0001501116 035 $a(PQKBManifestationID)11852317 035 $a(PQKBTitleCode)TC0001501116 035 $a(PQKBWorkID)11522208 035 $a(PQKB)11214962 035 $a(DE-He213)978-3-319-18203-2 035 $a(MiAaPQ)EBC2095726 035 $a(PPN)186028075 035 $a(EXLCZ)993710000000416821 100 $a20150530d2015 u| 0 101 0 $aeng 135 $aur|n|---||||| 181 $ctxt 182 $cc 183 $acr 200 10$aLandforms and Landscape Evolution of the Equatorial Margin of Northeast Brazil $eAn Overview /$fby Jean-Pierre Peulvast, François Bétard 205 $a1st ed. 2015. 210 1$aCham :$cSpringer International Publishing :$cImprint: Springer,$d2015. 215 $a1 online resource (198 p.) 225 1 $aSpringer Earth System Sciences,$x2197-9596 300 $aDescription based upon print version of record. 311 $a3-319-18202-1 320 $aIncludes bibliographical references at the end of each chapters and index. 327 $a1 Introduction -- 2 Geological setting: the Borborema Province -- 3 Morphostructural patterns -- 4 Stepped surfaces, palaeolandforms and morphostratigraphy -- 5 Late Cenozoic evolution of landforms -- 6 Conclusion and perspectives. 330 $aMore than a simple monograph, the authors present a comprehensive geomorphic overview of a large tropical region where they show how deciphering the long-term landform evolution helps understanding the present set of landscapes and morphodynamic environments. The Equatorial margin of the Brazilian ?Nordeste? displays stratigraphic landmarks whose interpretation reveals the age and nature of landforms, leading to a reconstruction of the geomorphic history by the means of combined morphostratigraphic and morphopedological approaches. Beyond the role of differential erosion related to moderate post-oceanic opening uplift, the plain and upland landscape reflects a juxtaposition of landform and soil generations related to a shallow basin inversion, the last stages of which occurred in semi-arid conditions since the Oligocene. These results throw light on old debates on models of long-term landform development in platform areas, and also help evaluating recent models of denudation and burial based on thermochronological methods. 410 0$aSpringer Earth System Sciences,$x2197-9596 606 $aGeomorphology 606 $aNatural disasters 606 $aGeomorphology$3https://scigraph.springernature.com/ontologies/product-market-codes/J16010 606 $aNatural Hazards$3https://scigraph.springernature.com/ontologies/product-market-codes/G32000 615 0$aGeomorphology. 615 0$aNatural disasters. 615 14$aGeomorphology. 615 24$aNatural Hazards. 676 $a551.410981 700 $aPeulvast$b Jean-Pierre$4aut$4http://id.loc.gov/vocabulary/relators/aut$01062814 702 $aBétard$b François$4aut$4http://id.loc.gov/vocabulary/relators/aut 801 0$bMiAaPQ 801 1$bMiAaPQ 801 2$bMiAaPQ 906 $aBOOK 912 $a9910299434103321 996 $aLandforms and Landscape Evolution of the Equatorial Margin of Northeast Brazil$92528645 997 $aUNINA