The ore-forming materials were mainly deprived from the host strata.
成矿物质主要来源于容矿地层。
The targets of further exploration are mainly underfault overthrust, strata fault compound, strata host anticlinal compound, host anticlinal ane solution lithologic traps.
深化勘探对象，主要为断下逆遮、地层-断层复合、地层-地垒背斜复合、地垒背斜和溶蚀岩性等圈闭。
Sulfur isotopic compositions of sulfides in the typical ore deposits hosted in different strata are on the whole consistent with those of Marine sulfates in corresponding host strata.
赋存于不同时代地层中的典型矿床的硫化物硫同位素组成，总体上显示出与容矿地层同期形成的海相硫酸盐硫同位素组成相一致的特征。
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