水热活动

其中川滇及缅甸西北部地区的Q0值最低（<240）.该地区地壳有复杂的断裂破碎构造及强烈的水热活动。

Yunnan , southwest Sichuan , and northwest Myanmar show the lowest Q_0 value ( Q_0 < 240 ) and the crust of these regions is characterized by complicated crack and strong hydrothermal activity .

闽南现今构造应力场与水热活动

Recent tectonic stress field and hydrothermal activity in South Fujian

中国东南部大陆边缘现代水热活动

Recent hydrothermal activity along the continental margin of Southeast China

腾冲火山地热区的水热活动显示强烈，小震微震活动频繁。

In the Tengchong volcano-geothermal region , there are strong surface expressions of hydro-thermal activities and frequent microseismicity .

根据地震的综合信息，探讨了研究区微震活动与水热活动的关系。

On the basis of these d ta , this article also gives a discussion on the relation between the microseismic activities and hydrothermal activities .

本文通过大量温泉资料的统计分析，探讨了滇西地区的水热活动特征。

The characteristics of the hydrothermal activity in West Yunnan region have been discussed through statistical analysis of a number of thermal spring data in this paper .

新建铁路大理至瑞丽线将以隧道形式通过水热活动强烈的高黎贡山区域，隧道可能会遇到高温水热危害。

Newly-built Dali-Ruili railway will get through Gaoligong Mountain areas in the form of tunnel , and may experience high-temperature heat and water hazards because hydrothermal activity is strong in tunnel zone .

区内近S&N向的主要大断裂和两组次一级的断裂是水热活动的主要通道和主要控热构造裂隙。

The major big rift and two groups of the minor rifts approximately pointing to S-N in the area are the main pathway and the main tectonic crack of heat controller for the hydrothermal activity .

论文对隧址区水热活动规律和地温场特征进行研究，这不仅能解决该区的基础地热地质问题，同时也可预测线路工程遇到的热害问题，具有实际意义。

Study on thermal activity and geothermal field characteristic in tunnel zone is of great significance , for it can not only solve basic geothermal geological problems but predict the heat-harm problems of the linear project .

经铀系法测定其水热活动的同位素年龄为14.6Ma左右，结合地层对比，认为水热活动时间为中更新世晚期。

The isotope age of the hydrothermal events determined by the Uranium-series methods is 14 . 6 Ma or so . Combined with the stratigraphic correlation , the time of the hydrothermal activity is considered to be Late Miocene-Pleistocene epoch .

催化裂化催化剂水热失活动力学模型

Kinetic model of hydrothermal deactivation for catalytic cracking catalyst

裂化催化剂水热失活动力学及装置平衡活性模型

Study on kinetic model of hydrothermal deactivation and model of unit balance activity for catalytic cracking catalyst

水热爆炸是活动性地热田的典型显示。

Hydrothermal explosions are a typical manifestation of active geothermal fields .

依据催化裂化催化剂水热失活过程伴随着超稳化过程，确定了催化剂自抑制水热失活动力学模型方程。

The kinetic model of hydrothermal deactivation and the model of unit balance activity for FCC catalyst were established .