Recessive
发表于 2025-3-26 21:53:37
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GULF
发表于 2025-3-27 04:13:41
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expound
发表于 2025-3-27 08:39:29
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FELON
发表于 2025-3-27 12:47:54
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
incontinence
发表于 2025-3-27 13:36:51
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NEEDY
发表于 2025-3-27 21:13:01
Ronald R. Rindfuss,Minja Kim Choe Because of the large surfaces covered by coarse debris at high altitudes, the granitic massifs of Retezat and Parâng present the most extensive areas with probable permafrost from the Southern Carpathians. Instead, the fine debris specific to crystalline ranges of Făgăraş and Iezer—Păpușa or the sm
GRIN
发表于 2025-3-28 00:55:22
Øystein 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
GIST
发表于 2025-3-28 02:48:04
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
Pelago
发表于 2025-3-28 10:08:06
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
无所不知
发表于 2025-3-28 12:22:43
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