半深海的

The sedimentary facies relating with carbonate rock include lakeshore, bank, bank margin, bathyal lake subfacies. 生物淺灘具有分布范圍廣闊、頂面平坦、進(jìn)積迅速、前斜坡明顯、沉積旋回發(fā)育、沉積厚度較小但穩(wěn)定的特征。

The Bibereck Formation of the Schmidsippl section in the type area of the Gosau Group (Northern Calcareous Alps, Austria) records a transgression and deepening of the depositional area from shallow neritic to bathyal depths. Schmidsippl剖面位于奧地利北鈣質(zhì)阿爾卑斯構(gòu)造帶內(nèi)Gosau群典型地區(qū)。 剖面出露的Bibereck組記錄了一個(gè)海侵和沉積區(qū)海水變深過程。

bathyal deposit 次深海沉積,半深海沉積

bathyal deposits 半深海沉積物