1) cathaysia landmass
华夏陆块
1.
It is a collision zone between Jiangnan landmass and Cathaysia landmass.
它是江南陆块与华夏陆块神功运动形成的碰撞拼贴带。
3) 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。
4) 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。
5) 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。
6) Cathaysia plate
华夏板块
1.
Penglu and Zhanggongshan micro-blocks occurred in the Huanan orogenic belt, which separated the Yangtze Plate from the Cathaysia Plate.
结合前人在区域构造和地质年代学的研究成果,认为晋宁运动时期,扬子板块东南缘散布着多个小型块体,在华夏板块向扬子板块方向的俯冲过程中,障公山地块先与彭庐地块沿程浪断裂带发生拼合,同时形成程浪超基性岩墙群;与此同时,彭庐地块内则表现为大规模的岩浆侵入作用。
补充资料：访陆处士羽（一作访陆羽处士不遇）
【诗文】：
太湖东西路，吴主古山前。所思不可见，归鸿自翩翩。
何山赏春茗，何处弄春泉。莫是沧浪子，悠悠一钓船。
【注释】：
【出处】：
全唐诗：卷816-26
太湖东西路，吴主古山前。所思不可见，归鸿自翩翩。
何山赏春茗，何处弄春泉。莫是沧浪子，悠悠一钓船。
【注释】：
【出处】：
全唐诗：卷816-26
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