Colorado Potential Geothermal Pathways

This layer contains the weakened basement rocks. Isostatic gravity was utilized to identify structural basin areas, characterized by gravity low values reflecting weakened basement rocks. Together interpreted regional fault zones and basin outlines define geothermal "exploration fairways", where the potential exists for deep, superheated fluid flow in the absence of Pliocene or younger volcanic units.

本层包含经弱化的基底岩石。通过静力重力法识别出结构盆地区域，这些区域以重力低值为特征，反映了基底岩石的弱化。结合区域断裂带和盆地轮廓的解释，定义了地热“勘探有利地带”，在这些地带中，在无上新世或更年轻火山单元存在的情况下，存在深层超热水流的可能性。