Sinian

基本解釋

The Tazhong uplift was an inherited palaeohigh evolved from Sinian Period.
塔中隆起是一個從震旦紀開始發(fā)育演化的繼承性古隆起。
What the ancient Indian people called as Sinian is China at present.
古代印度人稱的震旦就是今天的中國。
The major ore bed locates in the Doushantuo Formantion upper Sinian System.
礦體厚度品位沿傾向均有線性變化規(guī)律;
Hot event deposits occurred in Liantuo Formation of Lower Sinian, interbedded in fluvial facies sandstones and siltstones.
熱事件沉積產(chǎn)物見于下震旦統(tǒng)蓮沱組，夾于河流相沉積的砂巖及粉砂巖中。
This deposit occurs in Lower Sinian Nantuo sandstone at the exocontact zone of an Indosinian Dashenshan granite stock.
礦床產(chǎn)于印支期大神山花崗巖株外接觸帶之震旦系下統(tǒng)南沱砂巖組中。