ophiolite suite

基本解釋

The host rock belongs to volcanic rocks or volcanic-sedimentary rocks in the upper part of ophiolite suite;
容礦巖石為蛇綠巖套上部火山巖或火山— 沉積巖系；
The Ophiolite massifs are composed of mantle peridotite that is mainly harzburgite and dunite, and lacked of crust magmatite within the typical ophiolite suite.
該蛇綠巖帶的巖體由地幔橄欖巖組成，主要巖石類型是方輝橄欖巖和純橄欖巖，缺少典型蛇綠巖剖面中的洋殼單元。
Kudi ophiolite suite is composed of ultramafic rocks, gabbro, mantle source granitoid, basic volcanic rocks and flysch. It was formed during Sinian and Cambrian.
庫(kù)地蛇綠巖套由下部超鎂鐵質(zhì)巖、輝長(zhǎng)巖、幔源型花崗巖和上部基性火山巖、復(fù)理石等成分構(gòu)成，形成于震旦紀(jì)—寒武紀(jì)。