Tectonic uplift rates 地壳上升速度
cenozoic tectonic uplift 新生代构造抬升
tectonic uplift and subsidence belts 构造沉降带和隆起带
tectonic tilting uplift 构造掀斜隆升
Theformationandevolutionof sequencestratigraphyof Middle-Upper Jurassic series is affected by change of global sea level, tectonic uplift and subsidence, sedimentary supply and climate conditions.
中—上侏罗统层序地层的形成演化受全球海平面变化、构造隆升与沉降、沉积物供给以及气候条件的综合影响。
参考来源 - 青藏高原羌塘盆地东部中—晚侏罗世沉积相及层序地层分析Through integration analyse the periphery and inner Bohu sag uplift-chilling age of the basin, we confirmed the time limit of tectonic uplift-chilling event is 3762Ma(Eocene to Paleocene).
通过对盆地内部博湖南北坳陷抬升-冷却年龄的综合分析,确定盆地内部构造抬升-冷却事件的时限为37~62Ma(始新世到古新世)。
参考来源 - 焉耆盆地中新生代构造抬升与热演化研究·2,447,543篇论文数据,部分数据来源于NoteExpress
During Cenozoic, the most remarkable tectonic uplift in geologic history appeared as the result of material redistribution and adjustment in lithosphere.
新生代时,岩石圈中出现了物质的重新分配与调整,产生了地史上最为显著的构造隆升。
Mountains produced by the orogenic movement in the Mesozoic time and plateaus formed thereafter by tectonic uplift become an important factor that influences the global climate.
中生代造山运动造就的山脉和其后由构造隆升形成的高原,也是影响全球气候的主要因素之一。
The formation of sand waves is controlled mainly by underset of tidal current, and also related to tectonic uplift.
沙波形成主要受潮流底流的水动力作用控制,并与构造抬升有关。
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