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
Tectonic uplift and lateral compression are major factors responsible for the abnormal pressure.
本研究区异常高压形成的主控因素是构造抬升和水平构造挤压应力。
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。
Tectonic uplift and climate change are two key factors in controlling the development of river terraces in hinterlands.
构造运动和气候变化是制约内陆地区河流阶地发育的两个关键因素，而不同地区的河流对它们的响应方式多种多样。
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