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- Sinian dolomitite 震旦系白云岩
- The Tazhong uplift was an inherited palaeohigh evolved from Sinian Period. 塔中隆起是一个从震旦纪开始发育演化的继承性古隆起。
- What the ancient Indian people called as Sinian is China at present. 古代印度人称的震旦就是今天的中国。
- The major ore bed locates in the Doushantuo Formantion upper Sinian System. 矿体厚度品位沿倾向均有线性变化规律;
- Yuerya-type gold deposit occurs within the Yanshanian granite and its contact zone with Mesoproterozoic dolomitite. （2）产于中生代花岗岩中及其接触带中的峪耳崖式金矿；
- There is a series of strata composed of dolomitite, calcareous dolostone and quartzose sandstone. 大青山地区发育一套以白云岩、灰质白云岩和少量石英砂岩为主的地层。
- Hot event deposits occurred in Liantuo Formation of Lower Sinian, interbedded in fluvial facies sandstones and siltstones. 热事件沉积产物见于下震旦统莲沱组，夹于河流相沉积的砂岩及粉砂岩中。
- This deposit occurs in Lower Sinian Nantuo sandstone at the exocontact zone of an Indosinian Dashenshan granite stock. 矿床产于印支期大神山花岗岩株外接触带之震旦系下统南沱砂岩组中。
- There exist four layers of volcanic rocks in Sinian and Cambrian strata of Kuruktag area, Xinjiang. 在新疆库鲁克塔格地区的震旦纪和寒武纪沉积岩地层中，分布有四层火山岩。
- Taking Tarim and Qaidam basins of China for examples, the basins experienced three open-close cycles since Sinian. 对中国西北塔里木和柴达木盆地进行了多期叠合盆地油气运聚研究。
- It is hosted in the stratum of the group C of the Sinian system.Its deposit type belongs to the Niobium-Ta... 矿床赋存于震旦系C组地层中,中型规模,矿床类型为岩浆作用形成的白云母钠长石伟晶岩铌钽矿床。
- The uplift is an inherited mobile paleouplift that began its development and evolution in the Sinian. 此与塔里木盆地断裂构造体系的展布、基底结构与构造、地壳深部地质背景及古构造应力场演变等关系密切。
- This landslide is mainly composed of Sinian limestone and Cambrian carbon slate and phyllite. 该滑坡体主要由震旦系灰岩和寒武系炭质板岩、千枚岩构成。
- I called on Mr.Chen Yike in Nanjing, coming to Academia Sinica to visit Mr.Fu Sinian. 在南京曾叩见过陈寅恪先生，到中央研究院拜见过傅斯年先生。
- The whole Sichuan basin has developmental sedimentary covers and is deficient in only Devonian deposits above Sinian. 整个四川盆地沉积盖层发育，震旦系之上仅缺失泥盆纪沉积。
- The dolomite of Upper Sinian Dengying Formation is favorable ore-source rock and useful ore-preserving country rock. 上震旦统灯影组碎裂状白云岩是有利的矿源层及有利的赋矿围岩。
- The reefs widely developed from Sinian to Neogene in China, with main reef-forming stages in Devonian, Permian and Neogene, respectively. 摘要中国生物礁从震旦纪至新近纪均有发育，分布范围广，并有泥盆纪、二叠纪和新近纪3个主要造礁期。
- The gravity events include slumping event and turbidity-current event, and the gravity event deposits were developed in deep-water carbonate rocks in the Upper Sinian. 重力事件可分为滑塌事件和浊流事件，其沉积产物均分布于上震旦统，夹在大套的深水碳酸盐岩中。
- Emergence stratums are of Sinian、Devonian、Permian、Trias and intrusive Granite dike and coarse - grained granite dike. 出露地层为震旦系、泥盆系、二叠系、三叠系以及侵入的花岗岩脉和花岗伟晶岩脉。
- The allochthon consists of the Presinian,Sinian and Cambrian system.The autochthon comprises the Devonian and Carboniferous system. 推覆构造的外来系统为前震旦系、震旦系和寒武系，原地系统为泥盆系和石炭系。
