2) Moxi-Longnusi Area
磨溪-龙女寺地区
3) Zhongchuan area
中川地区
1.
Characteristics of fluid inclusions in the gold deposits within Zhongchuan area, western Qinling and their geological significance;
西秦岭中川地区金矿床流体包裹体特征及地质意义
2.
Zhongchuan area is located in the southern margin of the Li-Min forland basin which is caused by yangtze plate's subducting to Huabei plate,and it situated in the region between Lixian-taoping deep fault and its subfault Lixian-luoba fault.
西秦岭中川地区位于扬子板块向华北板块俯冲形成的前陆盆地南缘，深断裂带礼县—洮坪断裂带及其分支断裂礼县—罗坝断裂带所夹的区域内。
4) central Sichuan Basin
川中地区
1.
Thick-bed sand body genesis and oil-gas migration pathway in the forth member of Xujiahe Formation of Upper Triassic in the central Sichuan Basin;
川中地区上三叠统须四段厚层砂体成因及油气运移通道分析
2.
Genetic types and main controlling factors of sandbodies in second and fourth members of Xujiahe Formation,upper Triassic,Central Sichuan Basin;
川中地区上三叠统须二段和须四段储集砂体成因类型及其发育的主控因素
3.
Typical gas reservoirs and main controlling factors of reservoir-forming of Upper Triassic Xujiahe Formation in central Sichuan Basin
川中地区上三叠统须家河组典型气藏解剖与天然气成藏主控因素分析
5) middle of Sichuan basin
川中地区
1.
The paper mainly discussed the conditions of hydrocarbon accumulation in An Pingdian-Gao Shiti structure,middle of Sichuan basin.
本论文主要研究川中地区安平店—高石梯构造带震旦系—寒武系的油气成藏条件。
2.
The accumulation mechanism of natural gas is still an unsolved problem in the Lower Triassic Jialingjiang Formation of Moxi-Longnüsi area in the middle of Sichuan Basin.
川中地区磨溪—龙女寺构造带下三叠统嘉陵江组天然气的成藏机理一直是一个悬而未解的问题。
6) the area of middle-southeast of Sichuan baisn
川中-川东南地区
补充资料：玄中寺
| 玄中寺 中国佛教净土宗发源地之一。位于山西交城西北石壁山中。北魏昙鸾始建于延兴二年（472），并于此弘习净土学说。隋末道绰、唐代善导也曾住持此寺，并完成净土宗系统。日本净土宗及净土真宗均视此寺为其祖庭，并以昙鸾、道绰、善导为开宗的前三祖。 |
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