process of crustal movement 中文意思是什麼
process of crustal movement
解釋
地殼運動過程-
But self - organized criticality ( soc ) is a kind of weak chaos nature : " edge of chaos " ( non - stable steady state ), appearing only in the specific space - time region in specific stage at self organization process of crustal movement
「自組織臨界態」 ( soc )是一種弱混沌性質的「混沌邊緣態」 (非穩定定態) ,只出現于地殼運動自組織過程特定階段中的特定時空域。 -
After transient state process ( earthquake, etc ) having occurred, present - day crustal movement ( the changing process with time, the space distribution and the structure of spectrum ) will return to " stable steady state ( dynamic balancing state ) " voluntarily
在地震等暫態過程發生后,現今地殼運動(時變過程、空間分佈、頻譜結構)仍將自動回歸到「穩定態(動平衡態) 」 。
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