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1)  ridge segment
海岭块段
2)  block ridge
断块海岭
3)  submarine ridge
海岭
1.
The author considers that there are close relationships between the plane form of island-arcs and submarine ridges.
但其活动性在岛弧的延伸方向上及岛弧间存在明显的差异,表现在岛弧两端或岛弧与海岭的交接地段活动性较强,而中段活动性较弱。
4)  Qinling plate
秦岭板块
5)  Dongling Block
东岭区块
1.
Saturated Hydrocarbon Characteristics in Source Rocks and Palaeo-environment Significance in Dongling Block of Songliao Basin;
松辽盆地东岭区块烃源岩饱和烃特征及其古环境意义
2.
Evaluating maturity of source rocks by aromatic compounds:A case from Dongling Block,Songliao Basin
利用芳烃化合物评价烃源岩成熟度——以松辽盆地东岭区块为例
3.
Dongling block is located in the south-east of Changling County ofJinlin Province, and from angle of tectonic, it is located in the south ofcenter rift-subsidence section in Songliao basin, the south-east vicinitiesof Changling depression,and the south edge of Huazijing fault-uplift belt.
东岭区块位于吉林省长岭县东南部,构造上处于松辽盆地中央断陷区南部,长岭凹陷东南缘、华字井断凸带南端。
6)  east Nanling region
南岭东段
1.
Tungsten multimetals deposits in east Nanling region are famous mineralizationconcentrated region.
南岭东段是世界著名的钨多金属矿集中区,是由独特的地质环境构成多种类型的钨矿集中分布区。
补充资料:海岭
海底的山脉。一般较陆地的山脉高而长,而侧较陡。也叫海脊。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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