1) Lujiang-Zongyang

庐枞
1.
Tectonic setting of mesozoic magmatic activities in the region of Jingbian-Panzhuwa in Lujiang-Zongyang Volcanic Basin;
庐枞井边-盘珠洼地区中生代岩浆活动的构造背景
2) Lu-Zong region

庐枞地区
1.
Uranium and polymetals (iron and copper) constitute the regional metallogenetic seriesin Lu-Zong region,the metallogenesis of which is mainly controlled by regional gigantic deepfaults and pre-volcanic "basement" faults.
庐枞地区铀与铁、铜等多金属组成区域成矿系列,其成矿作用主要受区域性深大断裂及火山岩前“基底”断裂的控制,燕山期的岩浆活动及其演化是成矿的内在因素。
3) Luzong basin

庐枞盆地
1.
Majory and trace elements compositions of the syenite in the Luzong basin show that SiO2 contents of the syenite are 60.
研究了庐枞盆地正长岩类的时空分布规律,并对其地球化学特征和成因进行了探讨。
4) northern Lujiang-Zongyang basin

庐枞盆地北部
5) Luzong volcanic area

庐枞火山岩地区
6) Lujiang-Zongyang area in Anhui Province

安徽庐枞地区
1.
The Lujiang-Zongyang area in Anhui Province is located in the fault-depression zone of Lower Reaches of Yangtze River.
安徽庐枞地区位于下扬子断陷带内,区内中生代岩浆活动强烈,壳幔交换频繁,形成了一系列A型花岗岩类,其中产有一些同源岩石包体。
2.
Lujiang-Zongyang area in Anhui Province is located in the Lower reaches of the Yangtze River Fault-Depression Zone.
安徽庐枞地区位于下扬子断陷带内。
补充资料:枞枞
1.隆起貌;高耸貌。 2.排比貌。
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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