1) Caledonian
[英][kæli'dəuniən] [美][kælɪ'donɪən]
加里东
1.
Determination of the age of gold deposits in southeastern Guizhou: with a discussion of the Caledonian Hunan-Guizhou gold ore belt;
黔东南金矿形成时代的确定兼论湘黔加里东金矿带
2.
Tectonic evolution and sequence stratigraphic framework in South China during Caledonian;
加里东期华南的盆地演化与层序格架
3.
Using seismic, logging, and assaying data, and combined with vitrinite reflectance erosion thickness restoration method and seismic stratigraphy Paleogeomorphology restoration way, we have restored Caledonian paleogeomorphology in the central area of Tarim.
利用地震、测井和分析测试资料,结合镜质体反射率剥蚀厚度恢复法和地震地层学古地貌恢复法,对塔中地区中加里东期古地貌进行了恢复。
2) Caledonian
[英][kæli'dəuniən] [美][kælɪ'donɪən]
加里东期
1.
Caledonian karst palaeogeomorphology and the forming condition of gas pool,southern Ordos Basin;
鄂尔多斯盆地南部加里东期岩溶古地貌与天然气成藏条件分析
2.
Caledonian karstification of Ordovician carbonates in the Tahe oilfield,northern Tarim basin,Northwest China,and its petroleum geological significance;
塔里木盆地北部塔河油田奥陶系加里东期岩溶作用及其油气地质意义
3.
Chronological Study of Caledonian Metamorphic Pegmatite Muscovite Deposits in the Altay Mountains, Northwestern China, and Its Significance;
阿尔泰加里东期变质成因伟晶岩型白云母矿床的成矿年代证据及其意义
3) Caledonian Period
加里东期
1.
Systematical analysis of volcanism, sedimentation, magmatic intrusion, metamorphism and deformation in this area show that Suizhou-Yingshan area of Hubei Province during the Caledonian Period underwent five geological events which reveal a whole process of rifting and the Caledonian regional metamorphism is the last metamorphic event in Suizhou-Yingshan area.
通过综合分析随 (州 )应 (山 )地区加里东期火山 -沉积、侵入、变质和变形事件 ,总结出 5期地质事件 ,它们组成一个完整的地质事件序列 ,该序列反映出裂谷发生、发展到消亡的一个过程。
2.
There is a inherited paleouplift in the Jianghan Plain area of the southern margin of East Qinling and Dabie Orogenic Belt during Caledonian period.
加里东期在东秦岭—大别造山带南侧江汉平原地区存在一个继承性古隆起,前人所称的"鄂中古陆"是其具体的表现。
4) Caledonian orogeny
加里东运动
1.
9Ma,indicating the Yanwan intrusions formed at the end period of Late-Silurian and are the products of Caledonian orogeny in the late Paleozoic.
9Ma,属末志留世晚期,该侵入体应是早古生代晚期加里东运动碰撞造山过程的产物,其形成时代(414。
5) Caledonian movement
加里东运动
1.
Zircon La-ICPMS U-Pb Dating of the Weipu Granitic Pluton in Southwest Fujian and the Changpu Migmatite in South Jiangxi:Constrains to the Timing of Caledonian Movement in Wuyi Mountains
闽西南玮埔岩体和赣南菖蒲混合岩锆石La-ICPMS U-Pb年代学:对武夷山加里东运动时代的制约
2.
It is noted that the distinct function of Caledonian movement in this area is the formation of the linear migmatization and granitization on the basis of rift and tumescence basement.
本文提出武夷及其邻区存在两个裂陷槽及一裂隆，鹰潭－南城－安远－河源韧性断裂带为东部的火山岩型与西部的花岗岩型铀矿床的地质分界线，指出了加里东运动在本区的突出作用是使裂隆基底岩石发生混合花岗岩化作用。
3.
Through 1∶250000 regional geological mapping, many Caledonian tectonic deformation features and unconformable contact relationships at several sites were found in Sinian-Lower Paleozoic strata, indicating that Caledonian movement was strong in this area and that the Ca.
通过1∶25万区域地质填图,在震旦纪—下古生代地层中发现大量加里东期构造变形形迹和数处不整合接触关系,表明本区加里东运动强烈,华南地区广泛发育的加里东运动已经强烈地影响到扬子板块的南缘。
补充资料：加东
加东
新加坡 加东（katong）
位于东海岸一带的加东是一个环境幽静的居住区。早期住在这里的主要是富有的土生华人家族(“peranakan”在马来语中是“土生”的意思。土生华人、土生印度人和土生欧亚商社群是东南亚特殊历史背景下所形成的次族群)。这里的许多古老的土生华人房子以前曾是海边别墅，现在则因为填海的缘故而变得远离海边。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。