1) early to middle Ordovician
早中奥陶世
1.
In recent years,it discovered in the regional survey of the scale of 1∶50000 that the early to middle Ordovician absent in the southern Baoshan of western Yunnan.
近年的1∶5万区调工作发现,在滇西保山南部地区缺失早中奥陶世沉积,这是一个值得探索的重大地质问题,因为过去认为施甸地层小区的寒武-奥陶纪为连续沉积。
2) Early Ordovician
早奥陶世
1.
Analysis of momentary Characteristics and Evolution of Early Ordovician in Central Tarim Area.;
塔中地区早奥陶世沉积特征及沉积演化分析
2.
The carbonate storm deposit of early Ordovician Yeli Formation in Pingquan area, Hebei Province;
河北省平泉早奥陶世冶里组碳酸盐风暴沉积
3.
According to the analysis of sedimentary facies of Early Ordovician in Wudang,Guiyang,the authors suggest that the initial growth of Gaoyang fault took place in Early Ordovician and that the palae-fault experienced two revivals in the later tectonic movement.
根据贵阳乌当地区高院断层两侧早奥陶世地层的沉积相分析，首次提出了高院断层的最初形成时代为早奥陶世时期，在后期的构造运动中该古断裂发生了两次显著的复
4) Middle Cambrian-Early Ordovician
中寒武世-早奥陶世
5) Lower Ordovician
早奥陶世<地>
6) Middle Ordovician
中奥陶世
1.
Characteristics of Middle Ordovician Organic Reefs in Bachu Area;
巴楚地区中奥陶世生物礁造礁生物特征
2.
By means of core observation and log analysis of reservoir,it is recognized that widely distributed Tazhong uplift is formed from the late of Middle Ordovician to the early of Late Ordovician(from Llandeilo to Early Caradoc).
通过岩心观察、测井储集层分析等手段,识别出塔中凸起区广泛分布形成于中奥陶世晚期-晚奥陶世早期(兰代洛世-卡拉道克世早期)、发育于下奥陶统鹰山组中上部碳酸盐岩中且被上奥陶统良里塔格组覆盖的古潜山岩溶储集层,其原岩主要为开阔-半局限台地相颗粒灰岩、泥晶灰岩、藻灰岩夹白云岩。
3.
The middle Ordovician volcanic rocks of the Daliugou Group in the Hami-Wupu area of the Eastern Tianshan seem to be the oldest strata of the studied area.
新疆东天山哈密五堡地区中奥陶世大柳沟组是研究区出露的最老的火山岩地层,大地构造属于准噶尔板块-大南湖复合岛弧火山岩带。
补充资料：上陶恩
hohe tauern
奥地利南部，东阿尔卑斯山脉的一段。西起意大利边境齐勒塔尔山，东至卡奇山口，长110公里(70哩)。高峰林立，有奥地利最高点大格洛克纳山(grossglockner, 海拔3,797公尺〔12,457呎〕)。穿山公路有费尔伯陶恩(felber tauern)隧道和霍赫托尔(hochtor)隧道。有铁路穿过陶恩隧道(长8公里〔5哩〕)。以登山和滑雪闻名。
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