Levelheaded
发表于 2025-3-21 20:07:30
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ANTI
发表于 2025-3-21 23:49:39
Stephan Bröchler,Hans-Joachim Lauthot only past several statistical tests but also the test of physical plausibility. This evidence, both in the frequency and in the time domains, that orbital influences are felt by the climate system, implies that the astronomical theory might provide a clock with which to date old sediments with a
飞行员
发表于 2025-3-22 02:35:38
Ulrike Klinger example, and depending on research goals, the need for excavation may be precluded as when geophysical surveys provide accurate plans of buried architectural remains that offer sufficient information for cultural resource management purposes. Indeed, the simple mapping of architectural and other an
Nonflammable
发表于 2025-3-22 08:30:10
Sabine Kropp,Johannes Schuhmann which bears his name and announced that, contrary to official opinion, its surface was irregular and not smooth. We now know that this observation -and many others ofGalileo-was a correct one, but the opposition that always arises against research too far ahead of its time resulted in his condemnat
seruting
发表于 2025-3-22 10:05:00
Hans-Jürgen Bielingechnique. It holds much promise cellent efforts of such organizations as the Un for allowing us to use less energy and preserve derground Space Center of the University of more space for natural and human needs. It also Minnesota, the School of Architecture at Okla gives the individual and society
栏杆
发表于 2025-3-22 15:36:45
Roland Czadail engineering schools. Here the geotechnical instruction has been concentrated on soil mechanics and foundation engineering because foundation engineering has traditionally been the major component of geotechnical practice. Geotechnical special ists, however, generally have acquired considerable f
大暴雨
发表于 2025-3-22 17:55:45
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Proponent
发表于 2025-3-22 21:17:17
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沟通
发表于 2025-3-23 03:07:20
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旧石器
发表于 2025-3-23 06:10:18
Barbara Laubenthaltribution to the fault slippage in some regions. Also, the regional strain can only be relieved by movements in the lower crust and upper mantle. It is suggested that these movements almost certainly precede surface breakage. They could be detected by geodetic observations at 30-50 km from the fault