赦免
发表于 2025-3-28 15:31:12
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Pelago
发表于 2025-3-28 19:32:20
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符合你规定
发表于 2025-3-29 00:19:25
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Cabinet
发表于 2025-3-29 03:56:23
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candle
发表于 2025-3-29 10:31:27
Compressional and Shear Wave Velocities as a Function of Temperature in Rocks at High Pressure,relative variations of v. and v. with temperature in peridotite, eclogite, gabbro, granite, and quartzite are compared, and the velocity decrease in granite at the α/β-quartz inversion temperature is discussed with regard to low-velocity layers in the earth’s crust.
senile-dementia
发表于 2025-3-29 14:29:23
Some Petrophysical Aspects of Deep Structure,n on temperature distribution in the earth, as temperature is one of the main factors controlling resistivity. There are indications that the temperature is relatively low in the upper mantle. Because of the large scatter of the results the method is subjected to some uncertainty at the present stage.
FECT
发表于 2025-3-29 19:29:11
Gravity,. For the purposes of deep-seismic sounding only the regional anomalies are of interest. This map reflects the areas covered by young sediments as well as regions showing a decrease in thickness of the upper crust.
Inexorable
发表于 2025-3-29 22:39:27
Basic Data of the Deep-Seismic Sounding Observations,l Republic of Germany. As mentioned in the introduction, one of the most important aims of this monograph is to publish all data in such a form that they can serve as basic material for future detailed interpretation.
外星人
发表于 2025-3-30 00:04:23
Description of Profiles,d by the recording of quarry blasts. The arrangement of the profiles is mainly determined by the distribution of these quarry blasts. Additionally some special seismic-refraction investigations were performed. The data of the recording points are presented in tables.
calumniate
发表于 2025-3-30 04:46:29
Ultrasound of the Abdominal AortaThe results of refraction and reflection seismics and their interpretation with respect to the structure of the crust and upper mantle ought to be consistent with the appropriate results obtained by other geophysical methods. The papers in this chapter are presented to illustrate this point. They deal with the following subjects: