摘要
本文通过对福建省某些地层中的若干铅、锌、硫矿床的矿石结构构造进行研究,发现它们都具有同生沉积和后期改造的双重特征,结合矿床的其他地质特征.认为这些矿床的成因属于沉积改造型的层控矿床.
The present paper is focused on the research on the texture and structure of some Pb-Zn-S deposits in cercain strata in Fujian province. Double characteristics of syngenetic sediment and deuterogenic transform have be observed. On the basis of these characteristics and other information of the deposits it is deduced that these deposits belong to the type of stratabound deposit of sedimentary-transform in their origin.
出处
《福州大学学报(自然科学版)》
CAS
CSCD
1990年第3期118-122,共5页
Journal of Fuzhou University(Natural Science Edition)
关键词
铅矿
锌矿
硫矿
共生矿
成因
特征
ore fabric
syngenetic sediment
deuterogenic transform
stratabound deposit