1) nihowan sediment
泥河弯沉积(更新世)
2) mid-Pleistocene sedimentary strata
中更新世沉积地层
3) Holocene sedimentary
全新世沉积
1.
Holocene sedimentary of offshore and shallow sea and Xukou formation in Shandong are similiar in strata structures, vertical and transverse variation, sedimentary environment which formed in the same or similiar sedimentary environment and have similiar rock combination.
山东省近浅海全新世沉积与旭口组的地层结构、纵横向变化、沉积环境是相同或相似的沉积环境中形成的相似岩石组合。
4) late Devonian deposition
晚泥盆世沉积
1.
Also, it was in the pivotal period that Caledonina orogeny was transformed into Varis orogeny in late Devonian, Caledonian orogeny and its late stretch-rift event had been recorded in late Devonian deposition.
昆仑造山带基本构造-地层格架奠基于古生代,晚泥盆世是加里东造山旋回和华力西造山旋回转换的关键阶段,加里东碰撞造山和其后的伸展裂陷等记录均存在于晚泥盆世沉积地层中。
5) Early-Middle Devonian sedimentation
早-中泥盆世沉积
6) channel debris flow deposit
河道泥石流沉积
补充资料:更新世
更新世(约距今164万年前~约距今1万年前) Pleistocene Epoch 第四纪的第一个世,约开始于164万年前,结束于约1万年前。更新世时形成的地层称更新统,位于上新统之上 、全新统之下。1839年,英国C.莱伊尔把巴黎盆地含软体动物化石70%为现生种的地层称为更新世地层。更新统下限的确定见晚第三纪。 |
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
参考词条