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| 001 | vtls000559765 | ||
| 003 | RU-ToGU | ||
| 005 | 20210922090048.0 | ||
| 007 | cr nn 008mamaa | ||
| 008 | 170212s2015 gw | s |||| 0|eng d | ||
| 020 |
_a9783319182032 _9978-3-319-18203-2 |
||
| 024 | 7 |
_a10.1007/978-3-319-18203-2 _2doi |
|
| 035 | _ato000559765 | ||
| 040 |
_aSpringer _cSpringer _dRU-ToGU |
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| 050 | 4 | _aGB400-649 | |
| 072 | 7 |
_aRBGD _2bicssc |
|
| 072 | 7 |
_aSCI031000 _2bisacsh |
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| 082 | 0 | 4 |
_a551.41 _223 |
| 100 | 1 |
_aPeulvast, Jean-Pierre. _eauthor. _9466646 |
|
| 245 | 1 | 0 |
_aLandforms and Landscape Evolution of the Equatorial Margin of Northeast Brazil _helectronic resource _bAn Overview / _cby Jean-Pierre Peulvast, François Bétard. |
| 260 |
_aCham : _bSpringer International Publishing : _bImprint: Springer, _c2015. |
||
| 300 |
_aXIII, 186 p. 59 illus., 35 illus. in color. _bonline resource. |
||
| 336 |
_atext _btxt _2rdacontent |
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| 337 |
_acomputer _bc _2rdamedia |
||
| 338 |
_aonline resource _bcr _2rdacarrier |
||
| 490 | 1 |
_aSpringer Earth System Sciences, _x2197-9596 |
|
| 505 | 0 | _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. | |
| 520 | _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. | ||
| 650 | 0 |
_ageography. _9566247 |
|
| 650 | 0 |
_aNatural disasters. _9385291 |
|
| 650 | 0 |
_aGeomorphology. _9410702 |
|
| 650 | 1 | 4 |
_aGeography. _9566415 |
| 650 | 2 | 4 |
_aGeomorphology. _9410702 |
| 650 | 2 | 4 |
_aNatural Hazards. _9410701 |
| 700 | 1 |
_aBétard, François. _eauthor. _9466647 |
|
| 710 | 2 |
_aSpringerLink (Online service) _9143950 |
|
| 773 | 0 | _tSpringer eBooks | |
| 830 | 0 |
_aSpringer Earth System Sciences, _9410535 |
|
| 856 | 4 | 0 | _uhttp://dx.doi.org/10.1007/978-3-319-18203-2 |
| 912 | _aZDB-2-EES | ||
| 999 | _c414670 | ||