The fluid-geological map was made by combination of the characteristics of metallogenic fluids and the metallogenic conditions in terms of structural, stratigraphic and magmatic constraints.
将成矿流体的特征及构造、地层、岩浆岩等成矿条件综合反映到图上便形成了流体地质图。
2
Commonly, the isopachs, or contours that make up an isopach map, display the stratigraphic thickness of a rock unit as opposed to the true vertical thickness.