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Titlebook: Low Frequency Astrophysics from Space; Proceedings of an In Namir E. Kassim,Kurt W. Weiler Conference proceedings 1990 Springer-Verlag Berl

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發(fā)表于 2025-3-25 07:07:37 | 只看該作者
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發(fā)表于 2025-3-25 09:48:06 | 只看該作者
H. E. Payneof customary practices which certainly varied from county to county and sometimes varied within counties. Custom and Common Law had their limitations, however, in that initially they could not compensate the outgoing tenant for any improvements, nor did they allow for removal of any fixtures that mi
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A simple low-cost array on the lunar near-side for the early lunar expeditions,
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Status of low frequency radio astronomical allocations at the 1992 World Administrative Radio Confe
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發(fā)表于 2025-3-26 01:42:54 | 只看該作者
mazing patterns of folds, faults or fractures? Early geologists who understood all too well that most sedimentary rocks had been laid down as soft, horizontal layers have wrestled with questions such as these for centuries. Most educated Europeans during the medieval age until the 1700s were convinc
27#
發(fā)表于 2025-3-26 05:36:38 | 只看該作者
M. L. Kaiserarting with the most important process: weathering. Weathering takes place through a combination of both mechanical and chemical means. We have all experienced the results of weathering in day-to-day life whether you stumble over a tree root that broke the asphalt on your morning run or you hear the
28#
發(fā)表于 2025-3-26 12:27:13 | 只看該作者
Kurt W. Weilerarting with the most important process: weathering. Weathering takes place through a combination of both mechanical and chemical means. We have all experienced the results of weathering in day-to-day life whether you stumble over a tree root that broke the asphalt on your morning run or you hear the
29#
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發(fā)表于 2025-3-26 20:41:16 | 只看該作者
Harlan J. Smith large amounts of rock debris are responsible for the large inventory of glacial landforms. Even though we are living in a warm climatic period at the moment (the Holocene interglacial period), glaciers are still common in the cold climates of the higher latitudes as well as in high mountains all ov
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