1) Hing Tin Estate
兴田村
3) daxing mining field
大兴井田
4) Xinglong coalfield
兴隆煤田
1.
Thrust tectonics in the Xinglong coalfield and adjacent areas, northeastern Hebei, China, and its implications for regional tectonics;
河北东北部兴隆煤田区逆冲构造的特征及其区域构造意义
5) Taixing oilfield
台兴油田
1.
Study of reservoir sedimentary microfacies in lower subblock of Funing Formation of Paleogene in Taixing oilfield;
台兴油田下第三系阜宁组下亚段储层沉积微相研究
2.
Study and application of PVDF tubular ultrafiltration membrane to water treatment in low permeability oilfields——taking Taixing Oilfield as an example;
PVDF管式超滤膜在低渗油田水处理中的研究及应用——以江苏台兴油田为例
3.
Study on sedimentary microfacies of thin sandbody in Fu 3 member of Taixing Oilfield
台兴油田阜三段薄层砂体沉积微相研究
6) Xingcheng gas field
兴城气田
1.
Reservoir space type and control factors of the deep conglomerate reservoir in Xingcheng gas field;
兴城气田深层砾岩储层储集空间类型及控制因素
2.
Lithologic characteristics and provenance analysis of conglomerate in Ying-4 segment of Xingcheng gas field;
兴城气田营四段砾岩储层岩石学特征与物源分析
3.
Technical-economic Evaluation of Natural Gas Development in Volcanic Reservoirs in Xingcheng Gas Field of Songliao Basin
松辽盆地兴城气田火山岩储层天然气开发技术经济评价
补充资料：大兴隆起
北京活动构造带。斜贯北京小平原中部，呈北东走向，隐伏于地表之下。面积约为1300平方公里。大兴区域大部处于隆起的中部。其西北侧为北京凹陷，东南侧为燕郊－牛堡屯断裂、大厂凹陷，两侧分别以南苑－通州断裂带及永乐店－夏垫－马坊断裂带为界。南段与南各庄－长子营断裂、廊固凹陷为邻。隆起西北高而东南低，高点埋深仅几十米，位于黄村镇与南苑镇之间，形成于第三纪，上覆50～1000米左右的第三系和第四系地层，内幕是由中上元古界和古生界组成的蓟县系、青白口系、寒武系、奥陶系地层。次级背斜轴部在高点东向，约在榆垡－马驹桥一线。新生界地层由西北向东南逐渐加厚。大兴隆起的两侧有次一级的断裂下降活动，与北京凹陷相应，形成地垒式的构造。隆起的上部地表呈平原地貌形态。
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