Titlebook: Kohlenwasserstoff?le und Fette; sowie die ihnen chem D. Holde Book 1933Latest edition Julius Springer in Berlin 1933 Alkohol.Fette.Glycerid

Defect

書目名稱Kohlenwasserstoff?le und Fette影響因子(影響力)




書目名稱Kohlenwasserstoff?le und Fette影響因子(影響力)學科排名




書目名稱Kohlenwasserstoff?le und Fette網(wǎng)絡(luò)公開度




書目名稱Kohlenwasserstoff?le und Fette網(wǎng)絡(luò)公開度學科排名




書目名稱Kohlenwasserstoff?le und Fette被引頻次




書目名稱Kohlenwasserstoff?le und Fette被引頻次學科排名




書目名稱Kohlenwasserstoff?le und Fette年度引用




書目名稱Kohlenwasserstoff?le und Fette年度引用學科排名




書目名稱Kohlenwasserstoff?le und Fette讀者反饋




書目名稱Kohlenwasserstoff?le und Fette讀者反饋學科排名

除草劑

徹底明白

M. Naphtali,W. Bleyberg,G. Meyerheim,W. Manasse,K. H. Schünemannom any good consensus as to the origin of diamictites and pebbly mudstones. Glacial-marine deposits are surely widespread, both in time and space, but the very controversy that stems over their interpretation is an equally important point in stressing that high latitude seas are perhaps the most com

有惡意

habile

D. Holdeing the depositional setting. The low angle bedding and regional consistency of the bedrock seismic horizons within Hudson Bay allows detailed structure revealed by the Huntec DTS. high resolution system, to be extrapolated to depths where they are visible on the multichannel data. This approach has

Bone-Scan

AMOR

D. Holdeing the depositional setting. The low angle bedding and regional consistency of the bedrock seismic horizons within Hudson Bay allows detailed structure revealed by the Huntec DTS. high resolution system, to be extrapolated to depths where they are visible on the multichannel data. This approach has

搖曳

W. Bleyberg Helderberg Plateau demonstrated conclusively that the major cave systems had survived multiple glaciations in the Pleistocene. Comparison between marble caves in Norway and those in the northeastern US demonstrated much commonality of form and speleogenesis. Recent work has demonstrated glaciolacus

abolish

D. Holdeng clastics and eventually greatly deforming the Devonian carbonates along the Hudson River Valley. Other than Holocene calcareous tufa, no further carbonates were deposited on the region; clastic units of the Catskills migrated westward as the Alleghenian Orogeny ended the Paleozoic with the comple

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