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

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樓主: Defect
31#
發(fā)表于 2025-3-27 00:22:28 | 只看該作者
32#
發(fā)表于 2025-3-27 02:52:19 | 只看該作者
33#
發(fā)表于 2025-3-27 07:49:03 | 只看該作者
D. Holdehese are outlined in this paper. Unfortunately, most investigations of inferred glacial-marine sequences have relied on only a few of these criteria, and the criteria used vary with different investigators. Also, some major misconceptions about glacial-marine sedimentation exist; these are the resul
34#
發(fā)表于 2025-3-27 09:30:59 | 只看該作者
D. Holdetion of seismic reflection profiling systems. Data from Hudson Bay Canada, was concurrently collected using a Huntec DTS. high resolution subbottom profiler, a.6 litre (40 cubic inch) airgun with single channel seismic eel, and a 16 kilojoule sparker with multichannel seismic array. No detrimental “
35#
發(fā)表于 2025-3-27 14:57:28 | 只看該作者
D. Holdetion of seismic reflection profiling systems. Data from Hudson Bay Canada, was concurrently collected using a Huntec DTS. high resolution subbottom profiler, a.6 litre (40 cubic inch) airgun with single channel seismic eel, and a 16 kilojoule sparker with multichannel seismic array. No detrimental “
36#
發(fā)表于 2025-3-27 18:46:47 | 只看該作者
37#
發(fā)表于 2025-3-28 00:26:36 | 只看該作者
W. Bleyberg Vic Baker, Steve Egemeier, Ernst Kastning, John Mylroie, and Arthur and Margaret Palmer, all working in the Helderberg Plateau of central New York. They demonstrated that large, pre-glacial cave systems existed, and these caves had been modified by glaciation, primarily as a result of base-level ch
38#
發(fā)表于 2025-3-28 04:54:08 | 只看該作者
D. Holde (including the Grenville Marble) of the Adirondack Mountains was formed during the assembly of the supercontinent of Rodinia. Cambrian and early Ordovician carbonates, along with clastics, were deposited in continental shelf conditions until the mid-Ordovician Taconic Orogeny, when those carbonates
39#
發(fā)表于 2025-3-28 07:11:05 | 只看該作者
D. Holdedeveloped in Cambro-Ordovician marbles to the east and southeast, and from caves in Siluro-Devonian carbonates to the south (deformed) and southwest (undeformed). This cave region is understudied and little scientific work has been done, although a limestone pavement project and a maze cave examinat
40#
發(fā)表于 2025-3-28 14:02:57 | 只看該作者
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