Science. 1979 Jul 6;205(4401):90-3. doi: 10.1126/science.205.4401.90.
Three large Venus surface features, identified previously in images obtained from Earth-based radar observations, are shown by the Pioneer Venus radar mapper to be elevated 5 to 10 kilometers above the surrounding terrain. Two of these features, one bright and the other dark, lie adjacent to each other astride the 65 degrees N parallel between longitudes 310 degrees E and 10 degrees E. The combined region forms a huge tectonically uplifted plateau, surmounted by radar-bright ridges that may have either a volcanic or tectonic origin. The third feature, located at 30 degrees N, 283 degrees E, is radar-bright and may consist of volcanic material extruded along a fault zone. A first radar-scattering image, compiled from data obtained by the mapper in its imaging mode, shows a region north of the equator; several circular depressions seen in this area may result from meteoritic impact.
先驱者金星雷达测绘器显示,金星表面三个先前在地球基地雷达观测图像中识别出的大型地貌特征高出周围地形 5 到 10 公里。这两个地貌特征,一个明亮,另一个黑暗,彼此相邻,横跨东经 310 度至东经 10 度、北纬 65 度之间的平行线。这两个地貌特征所在区域形成了一个巨大的构造隆起高原,上面耸立着雷达亮的山脊,可能具有火山或构造起源。第三个特征位于北纬 30 度、东经 283 度,雷达亮,可能由沿断裂带挤出的火山物质组成。测绘器在成像模式下获取的数据编译而成的首张雷达散射图像显示了赤道以北的一个区域;该区域中看到的几个圆形洼地可能是由陨石撞击造成的。