Morsel
发表于 2025-3-26 23:28:24
also depends on factors other than state variables, such as grain size, dislocation density, and especially time (rate of heating, duration of annealing, rate of cooling). Extrapolation of kinetic data obtained at high temperatures on laboratory time scales to more realistic lower tempera tures and geologica978-3-642-76147-8978-3-642-76145-4
gruelling
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擦试不掉
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SOW
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Stress
发表于 2025-3-27 15:57:25
https://doi.org/10.1007/978-94-009-3569-3Clastic minerals of the Appin Quartzite are: ca. 85 vol % quartz, ca. 15% alkali feldspars, heavy minerals (zircone, rutile — partly formed from titanomagnetite during diagenesis, and apatite and tourmaline as very rare exceptions.
Pander
发表于 2025-3-27 21:46:08
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SAGE
发表于 2025-3-28 01:10:26
Florencia Riegelhaupt,Roberto Luis CarrascoOxygen isotope fractionation between coexisting minerals may indicate equilibrium or disequilibrium, provided the temperature of formation is known. Depending on the time of blocking of specific .O/.O ratios, the fractionations contain information on:
顶点
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Narrative
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Hemodialysis
发表于 2025-3-28 10:55:46
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