MODE
发表于 2025-3-30 09:27:48
Introduction to Modern Electrochemistry,ic operations is designed, to interpolate the middle layer configuration from two serial sections. A conditional skeleton operation plays a key role to outline the middle layer. The method was applied to reconstruct the three-dimensional pore geometry of rocks.
Proponent
发表于 2025-3-30 13:51:57
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客观
发表于 2025-3-30 16:47:03
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领袖气质
发表于 2025-3-30 21:31:14
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visceral-fat
发表于 2025-3-31 02:23:09
,Three-dimensional reconstruction of pore geometry from serial sections—Image algebraic approach,ic operations is designed, to interpolate the middle layer configuration from two serial sections. A conditional skeleton operation plays a key role to outline the middle layer. The method was applied to reconstruct the three-dimensional pore geometry of rocks.
Neutral-Spine
发表于 2025-3-31 06:29:03
Computer graphics techniques to represent volcanic hazard and risk,sed as background for numerical result representation. Moreover both the cases of static results and time-dependent data have been considered. In the last case, dynamic animation has been adopted to show system evolution. Applications are presented for tephra fallout risk, lava flow hazard and lahar flowing.
Accord
发表于 2025-3-31 11:43:52
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LEERY
发表于 2025-3-31 15:49:31
Developments in Input-Output Analysisinhomogeneous elastic plate, involving the buoyancy force of the underlying conventional basin analysis techniques. As an example application, the development of a delta was modeled over one million years and the resulting stratigraphic sequence was then buried beneath 3,000 meters of sand-rich sediments.
anatomical
发表于 2025-3-31 18:47:49
https://doi.org/10.1007/978-3-319-51556-4terpretation. The use of parametric curves and surfaces provides a compact and editable representation of the geometry allowing the interpreter to quickly modify the model when new data becomes available or alternative “realizations” are required.
recede
发表于 2025-3-31 21:44:29
,Stanford’s sedsim project: Dynamic three-dimensional simulation of geologic processes that affect cIM appears to be reasonably effective in representing flow and sedimentation in meandering channels, and should provide insight in understanding the spatial distribution of sediment bodies in fluvial deposits and the internal structures within these bodies.