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Titlebook: Low Fertility, Institutions, and their Policies; Variations Across In Ronald R. Rindfuss,Minja Kim Choe Book 2016 Springer International Pu

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發(fā)表于 2025-3-26 21:53:37 | 只看該作者
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發(fā)表于 2025-3-27 12:47:54 | 只看該作者
o fertility, based on survey data, and government support for families. This broad overview, along with a general introduction, helps put the specific country papers in context.?. .As birth rates continue to de978-3-319-81417-9978-3-319-32997-0
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發(fā)表于 2025-3-27 21:13:01 | 只看該作者
Ronald R. Rindfuss,Minja Kim Choe Because of the large surfaces covered by coarse debris at high altitudes, the granitic massifs of Retezat and Parang present the most extensive areas with probable permafrost from the Southern Carpathians. Instead, the fine debris specific to crystalline ranges of F?g?ra? and Iezer—P?pu?a or the sm
37#
發(fā)表于 2025-3-28 00:55:22 | 只看該作者
?ystein Kravdalion of geomorphosites. Several methods amongst the most widely used in the literature (Pralong in Géomorphol Relief Processus Environ 3:189–196, .; Coratza and Giusti in Il Quaternario 18(1):307–313, .; Bruschi and Cendrero in Il Quaternario 18(1):293–306, .; Serrano and Gonzalez-Trueba in Géomorpho
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發(fā)表于 2025-3-28 02:48:04 | 只看該作者
Olivier Thévenone model along cuesta scarp slopes; this is mainly related to the lithology dominated by limestones, sandstones, and volcanic consolidated tuffs at the upper part of the slopes, with friable clayey and sandy strata intercalations. The landslide inventory and the revealed types and patterns of landsli
39#
發(fā)表于 2025-3-28 10:08:06 | 只看該作者
Wendy SigleM late phase (20–21?ka), up to three glacial readvances during the Oldest Dryas (18.6, 16.3 and 15.0?ka), one possible glacial advance during the Older Dryas (around 13.5?ka), a Younger Dryas glacial advance at 12.9–12.1?ka and a last possible glacial phase with isolated small glaciers and glacieret
40#
發(fā)表于 2025-3-28 12:22:43 | 只看該作者
Sarah R. Brauner-Ottobly in diachronic ways. The Neogene clastic sedimentation on piedmonts and coastal areas mainly reflects the occurrence of dry periods inducing widespread stripping of deep soil horizons and erosion of bare rock slopes and surfaces. Dissection stages occurred in periods of more humid climate and/or
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