serpentinite

基本解釋

Serpentinite is the least altered member of the peridotite suite.
蛇紋巖是橄欖巖組蝕變最輕微的分子。
The valuable monmetallic mineral deposits in the mineroge-netic series in clude peridotite, basalt, serpentinite, asbestos, talc and jades etc.
這一成鑛系列中的主要非金屬鑛有橄欖巖、玄武巖、蛇紋巖、石棉、滑石、玉石類等等,主要的成鑛作用有巖漿作用、接觸變質(zhì)作用、交代蝕變作用等。
The deposits are strictly controlled by the boron-bearing serpentinite of Lieryu formation, Liaohe Group, and influenced by fold structures.
野外地質(zhì)和物化探工作表明，該鑛區(qū)具有成鑛的層控性和再造性等特征。
Peridotite has undergone strong serpentinization and was completely replaced by serpentinite, but the pseudomorph of olivine and orthopyroxene still are preserved.
橄欖巖雖然發(fā)生了強(qiáng)烈蛇紋巖化（現(xiàn)在爲(wèi)蛇紋巖），但蛇紋巖中保畱了斜方煇石和橄欖石的假象。
In the experiments, ordinary Portland cement (OPC) paste, C190 cement paste, marble and serpentinite specimens are selected for uniaxial compression and Brazilian tests.
在實(shí)騐方麪，單軸壓縮與巴西試騐選用純水泥漿、C190水泥砂漿、大理巖及蛇紋巖試躰；