1) Tarim landmass
塔里木陆块
2) Tarim block
塔里木地块
3) Tarim plate
塔里木板块
1.
Sedimentary response to the Early-Mid Permian basaltic magmatism in the Tarim plate;
塔里木板块早—中二叠世玄武质岩浆作用的沉积响应
2.
The Characteristics of basic-ultrabasic rocks in the back-arc rift system on the northeastern margin of the Tarim plate;
塔里木板块东北边缘弧后裂谷系统基性、超基性岩特征
3.
The monzogranite has a single ziron U-Pb age of 245±6Ma, indicating that the collision suture between North China and Tarim plate was formed during Late Permian.
从宏观地质学、岩石矿物学、地球化学、包体特征并结合区域资料分析 ,晚二叠世赛里超单元属于同碰撞且以结构演化为特征的二长花岗岩超单元 ,其颗粒锆石 U-Pb年龄为 ( 2 45± 6)Ma,从另一角度说明了该地区晚二叠世时华北板块与塔里木板块的碰撞缝合。
4) Tarim paleo-plate
塔里木古板块
1.
The correlation of evolutions between Yangtze paleo-plate and Tarim paleo-plate was analyzed using the petrology of orogenic belt in the edge of plate.
板块边缘造山带的岩石学记录追踪了扬子与塔里木古板块地史演化中的相关性,从岩石学、古气候学和古生物学等方面论证了扬子与塔里木古板块内部地质特征的可比性。
2.
In this paper we demonstrate that the geological characteristics between the Yangtze and Tarim paleo-plates, based on petrology, paleoclimatology and paleontology research, are comparable.
在前人有限资料基础上,从岩石学、古气候学和古生物学等方面,论证扬子与塔里木古板块内部地质特征的可比性,从构造解析板块边缘造山带的岩石学记录,追踪扬子与塔里木古板块地史演化中的相关性,得出从新元古代至二叠纪扬子古板块多与塔里木古板块靠近,成为一个大陆,我们暂命名为“塔里木-扬子古大陆”。
5) Tarim micro-plate
塔里木微板块
1.
Geochemistry and their tectonic significance of the volcanic rocks from Tarim micro-plate;
塔里木微板块震旦-寒武系火山岩地球化学及其大地构造意义
6) the south margin of the Tarim plate
塔里木板块南缘
1.
Following the Sinian paleogeographic pattern, the south margin of the Tarim plate in the early Paleozoic period was in neritic shelf bathyal milieu, in which deposited a set of strata composed of marine carbonate rocks and detrital rocks.
塔里木板块南缘早古生代时期继承了震旦纪的古地理格局 ,处于浅海陆棚—半深海环境 ,沉积了一套海相碳酸盐岩和碎屑岩地层。
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