The natural thermoluminescence in Quaternarysediment has stored accumulated irradiated dose since the sediment deposited.
第四纪沉积物的天然热释光中储存有自沉积以来的累积辐射剂量。
2
So it is possible to determine a sitting of fault covered with Quaternarysediment and its activity by means of measurement of mercury-vapour containt.
观测结果可用来确定第四纪沉积物复盖区断裂的位置和可见断裂的活动性。
3
The most important conclusion is that the site magnifying effect is decided mostly by media parameters. It is larger in Quaternarysediment and shows different on Z and R components.