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根据围绕蚀变中心的特定金属矿床分带,可以区分某种矿化温度范围的矿物分区。将相似地区按照温度-共生次序排列,分划出相邻的线状区域带,就能建立区域分带和横切此带的矿化温度-强度的梯度。矿物带与围绕大陆活动带的挤压(造山)和张裂(地裂运动)构造活动期的变形强度带一致。矿化强度的梯度同变形强度梯度是吻合的。所以,可以认为每个构造旋回期能够形成一个同期矿化旋回,或稍晚的矿化旋回。据信,浅成造山运动的摩擦热能使垒部有用的地表流体一起汇入热液流体。根据成矿元素的温度稳定性,达种流体可使它们发生淋滤、运移和再分配,从而产生区域分带。地裂作用主要发生于低温元素处于激发状态的后陆(hinterland,或译后置地),孕育出深断裂,这些断裂可进入到地幔,并导入新的元素,包括低温稳定的新元素。铀在最低温环境中最为稳定。因此,在两种类型矿化梯度的前陆(foreland,或译前置地)前端可寻找出区域分带的位置。这种在整个美洲活动带中关系的一致性,证明可推广到垒世界任何年代的活动带,以达到预测铀成矿区的目的。在早期完成的有关伊此利亚半岛成矿构造的解释,表明铀已迁移到可能在梅塞塔高地中部的低温环境中。在那里已发现有第三纪的铀矿床。在没有矿床成因资料的情况下,根据活动带的构造分析预测了世界共余地区最宜于铀矿生成的区域位置。用这种方法得知的最有利区域,包括了世界上已知的最有意义的铀矿区。
Depending on the zoning of a particular metal deposit surrounding the alteration center, it is possible to distinguish mineral zones of a certain mineralization temperature range. By aligning similar areas in a temperature-symbiotic sequence and dividing adjacent linear zones, a regional tectonic gradient and a gradient of mineralization temperature-intensity across this zone can be established. The mineral zones are consistent with the deformation intensity bands during the tectonic movement of the compression (orogeny) and the fault (earth-fissure movement) around the continental belt. The gradient of mineralization intensity is consistent with the gradient of deformation strength. Therefore, it can be considered that each tectonic cycle can form a contemporaneous mineralization cycle or a later mineralization cycle. It is believed that the frictional heat of the shallow orogeny makes the useful surface fluids of the basins merge into the hydrothermal fluids. Depending on the temperature stability of the metallogenic elements, reaching fluids can leach, migrate, and redistribute them, resulting in zone zoning. Ground-cleavage mainly occurs in the hinterland (or translocation) where the low-temperature elements are excited to breed deep faults that can enter the mantle and introduce new elements, including new elements that are stable at low temperatures. Uranium is the most stable in the lowest temperature. Therefore, the location of zonation of the area can be found at the foreland of both types of mineralized gradients. This coherence of relations throughout the zone of activity in the Americas shows that it can be extended to any activity zone in the base world in order to achieve the purpose of predicting uranium metallogenic zones. An early explanation of the mineralization in the Ilica Peninsula, completed earlier, shows that uranium has migrated to a low temperature environment that may be in the middle of the Meitailheigh. There have been found in the Tertiary uranium deposits. Based on the tectonic analysis of the active zones, we predict the most suitable regional locations for uranium deposits in the rest of the world without deposit genetic information. The most advantageous areas known in this way include the most significant uranium deposits known in the world.