Science. 1969 Aug 29;165(3896):897-9. doi: 10.1126/science.165.3896.897.
Earthquakes instrumentally recorded from 1966 to 1968 have occurred in the same regions of western Colorado, the Arkansas and Platte river valleys, as those felt back to 1870 (from newspaper reports), despite the increasing cultural effects of mining, highway construction, reservoir building, and loading. Thus it appears unnecessary to explain the Denver earthquakes in terms of pressure induced by the introduction of waste fluid. However, the assumption of preexistent tectonic strains in the area of the Rocky Mountain Arsenal seems to be confirmed.
1966 年至 1968 年仪器记录的地震发生在科罗拉多州西部、阿肯色河和普拉特河谷地区,与 1870 年以来(根据报纸报道)感觉到的地震相同,尽管采矿、公路建设、水库建设和装卸等人为活动的影响日益增强。因此,用引入废液产生的压力来解释丹佛地震似乎没有必要。然而,洛基山兵工厂地区存在先前构造应变的假设似乎得到了证实。