1) Cathaysia
“华夏古陆”
1.
Questions to "Cathaysia Old Land", "Cathaysia Block" and "United Yantze-Cathaysia Old Land" of South China;
对“华夏古陆”、“华夏地块”及“扬子-华夏古陆统一体”等观点的质疑
2.
Grabau proposed“Cathaysia”concept several gencration geologists of China had revealed numerous important geological phenomena concerned,but it is still not sure if“Cathaysia”exists.
自葛利普创名“华夏古陆”以来,经过半个多世纪的论辩与考订,对其地质构造属性,至今仍然否定与肯定交迭起伏,莫衷一是,本文从推覆构造,陆地漂移等实际资料着手, 加以论证,认为它是经历深刻改造和发生巨大位移的变质岩断片体,地质构造属性已非“华夏古陆”原义。
2) Cathaysia
华夏古陆
1.
Highly precise zircon SHRIMP U-Pb dating was carried out on granitic gneiss in the Late Precambrian Yunkai metamorphic complex, garnet pyroxenite in the medium- and high-grade metamorphic Tiantangshan Group complex and mid-ocean ridge metabasic volcanic rocks (amphibolite) in the medium- and low-metamorphic Yunkai Group complex in the Yunkai area, Guangxi, southwestern Cathaysia.
对位于华夏古陆东南部的广西云开地区大面积出露的晚前寒武纪变质杂岩中的主体花岗质片麻岩、中深变质的天堂山岩群石榴辉石岩和中浅变质的云开岩群洋中脊型变质基性火山岩(斜长角闪岩)进行了高精度锆石SHRIMP U-Pb定年。
2.
Dating and study on genesis of the Mamianshan Group are important approach tocharacterize the Zhenghe-Dapu deep fault zone, and to better understand the formation and evolu-tion of the Cathaysia block.
马面山群是华夏古陆上裂谷环境的产物。
3.
In this paper, the author tentatively sums up the present situation of studying and the respective different opinions concerning Cathaysia, magmatectonic activity and geologic structure in the current fundamental geology surveying and research in Fujian province, and discusses simply their further studying orientatio
就当前福建基础地质调查研究中涉及的华夏古陆、岩浆构造活动、地质构造等有关问题研究现状及各自不同认识作初步归纳 ,并对其进一步研究方向作粗浅探讨。
3) Cathaysian old land
华夏古陆
1.
The Cathaysian old land proposed by A.
葛利普1924年创立的华夏古陆,是指震旦纪至侏罗纪时期位于华夏地槽以东并高出海平面的古陆地,主要分布于现今粤闽中东部和浙南东部经东海延达日本东北部海域,是晨旦纪至早古生代华夏地槽沉积的主要物源区。
4) Cathaysia Block
华夏古陆
1.
The Paleoproterozoic amphibolite of (1766±19)Ma in the SW Zhejiang and NW Fujian provinces, the Cathaysia block, has ε Nd ( t ) values ranging from +5.
华夏古陆闽浙地区古元古代晚期（（１７６６±１９）Ｍａ）斜长角闪岩的εＮｄ（ｔ）值变化范围为＋５。
2.
Deochemical data and SHRJMP U-Pb zircon isotopic age of (1766±19)Ma are reported for the amphibolites exposed in NW Fujian-SW Zhejiang and genetally accepted as the oldest rocks in the Cathaysia Block.
77Ga前发生了广泛的板内玄武岩浆活动，华夏古陆很可能是在古元古代晚期由太古亩地壳再循环物质重熔结晶克拉通化而形成的。
5) Yangtze-Cathaysia
扬子-华夏古陆
6) Sarcocheilichthys sinensis blecker
华
参考词条
补充资料：次韵陆友仁吴中览古
【诗文】：
赤阑桥下记停桡，细雨菰蒲响莫潮。
说与行人莫回首，故宫烟柳正萧萧。
【注释】：
【出处】：
元诗别裁集
赤阑桥下记停桡，细雨菰蒲响莫潮。
说与行人莫回首，故宫烟柳正萧萧。
【注释】：
【出处】：
元诗别裁集
说明：补充资料仅用于学习参考，请勿用于其它任何用途。