1) superlandmass
超陆块
2) continental block
陆块
1.
The continental block of Xinjiang and its adjacent areas was broken up in the late Cambriantime.
显生宙初，新疆曾是一个统一的陆块。
2.
Tectonic configuration,collage of small continental blocks with large passive margin may have contributed to the formation and development of remnant basin.
残余洋盆是板块拼合碰撞过程中残留的、未彻底闭合的洋盆,为碰撞陆块之间最晚闭合的区域。
3) land masses
陆块;地块 LM
4) North China Block
华北陆块
1.
Geological Character and Potential Resources of Iron Deposits in the North China Block;
华北陆块铁矿床地质特征和资源潜力展望
2.
The Tectonic Systems of Ore Control of the Gold Metallogenic Focus-Area in the Middle North Margin of North China Block;
华北陆块北缘中段金矿床密集区控矿构造
3.
Analysis on the Lithofacies and Paleogeography of Fengtai Group in the Southeast North China Block;
华北陆块东南缘凤台组岩相古地理分析
5) jiangnan landmass
江南陆块
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。
6) 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。
补充资料：陆俊超
上海人。幼年侨居印尼、马来西亚、新加坡，历任水手、管理员、轮船驾驶员，1946年回国后任上海工运局船长。1956年开始发表作品。著有长篇小说《幸福的港湾》，短篇小说集《姐妹船》、《国际友谊号》，选集《相逢在安特卫普》等。
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