Science. 1967 Nov 3;158(3801):641-2. doi: 10.1126/science.158.3801.641.
Material of basaltic composition at the Surveyor V landing site implies that differentiation has occurred in the moon, probably due to internal sources of heat. The results are consistent with the hypothesis that extensive volcanic flows have been responsible for flooding and filling the mare basins. The processes and products of lunar magmatic activity are apparently similar to those of the earth.
勘测者 V 着陆点的玄武岩成分表明月球发生了分化，这可能是由于内部热源造成的。这一结果与广泛的火山喷发导致月海盆地充满熔岩的假说相符。月球岩浆活动的过程和产物显然与地球的相似。
