tectonic discontinuity 中文意思是什麼
tectonic discontinuity
解釋
構造不連續面- tectonic : adj. 1. 構造的；建築的。2. 【生物學】構造的。3. 【地質學；地理學】地殼構造上的，起因於地殼運動的。
- discontinuity : n. 1. 斷絕，中斷；間斷。2. 【物理學】不連續性，突變性，突變點；【數學】不連續點；斷續函數。
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The structure also control the formation of large and super - large deposits, which commonly lie in the cross of different directions fractures or contacting belts of different tectonic units. 4. as a whole, gradient belts of moho discontinuity correspond to rock bodies, the flat area correspond to basement
4 、總體上，莫霍面的陡度帶一般與巖體相對應，莫霍面的平緩區與基底具有較好的對應關系，大型、超大型礦床一般分佈在莫霍面的陡度帶_上。 -
To calculate this boundary parameter, mohorovicic discontinuity palaeo - heat flow value during basin evolution process is identified through geotectonic background analogy method based on " peeling " method model, and the basin basement palaeo - heat flow is calculated through inversion from today to antiquity with current tectonic structure as constraint condition for palaeo - crustal architecture analogy
為了求取這個邊界參數，以「剝層」法模型為基礎，通過大地構造背景類比法確定盆地演化過程中莫霍面古熱流值，以現今地殼結構為約束條件類比古地殼結構，從今至古反演求取了盆地基底的古熱流。
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