2) Fushan sag
福山凹陷
1.
Gravity flow deposits of Paleogene Liushagang Formation in Fushan Sag,Hainan Province;
海南福山凹陷古近系流沙港组重力流沉积研究
2.
Sedimentary facies of the Liushagang Formation of Paleogene in Fushan Sag of Hainan Island;
海南岛福山凹陷古近系流沙港组沉积相
3.
The seismic data and drilling data are used to analyze the distribution of igneous rock in Fushan sag.
根据钻井和地震资料,分析了海南福山凹陷火成岩的分布特征,认为该地区火成岩有3种类型,即:分布于地表的喷发岩、次火山相火成岩、深层侵入岩。
3) Fushan depression
福山凹陷
1.
Reservoir controlling mechanism and petroleum accumulation model for consequent fault and antithetic fault in Fushan Depression of Hainan area;
海南福山凹陷顺向和反向断裂控藏机理及油气聚集模式
2.
A discussion on the Palaeogene sublacustrine fan of Fushan depression in Beibuwan basin, northern South China Sea;
北部湾盆地福山凹陷古近纪湖底扇沉积演化及模式探讨
3.
By using(δ~(13)C_2-δ~(13)C_3) versus C_2/C_3(mol/mol) plot and "natural gas plot",and the ternary diagram of C_7-hydrocarbon of natural gas,this paper studies the genesis and source of the natural gas discovered in the Fushan depression,Hainan.
利用(1δ3C2-1δ3C3)-C2/C3(mol/mol)关系、“天然气曲线”和天然气C7-重烃三角图对海南福山凹陷天然气的成因和来源进行了研究,结果表明福山凹陷天然气主要为干酪根生烃高峰到湿气阶段的产物;天然气和该区原油同源,都来自流沙港组Ⅱ-Ⅲ型有机质;天然气没有遭受明显的次生变化,受运移效应的影响也较弱;花场地区天然气主要来自白莲次凹,而Hx4井和H 3-4井的天然气可能有来自皇桐次凹的贡献。
4) piedmont depression
山前凹陷
1.
The geotectonic position of study area lies in the southern margins of the Zhungeer depression and Dalongkou depression, which belong to the Urumchi piedmont depression.
研究区大地构造位置位于乌鲁木齐山前凹陷(Ⅲ2)之准噶尔南缘凹陷(Ⅳ3)和大龙口凹陷(Ⅳ5)内。
5) Yingshan sag
莺山凹陷
1.
It is believed that the Yingshan sag,a kind of large-scale deep sag under the control of transtensional faults,is another target for deep gas exploration following the Xujiaweizi depression.
通过二维、三维地震连片解释,落实了断陷结构和构造格局,结论认为:莺山凹陷为构造深凹区,规模较大,受张扭性断裂控制,是继徐家围子之后深层天然气勘探的主力接替区。
6) xiaoban Depression
小板凹陷
补充资料：凹陷骨折
凹陷骨折
depressed fracture
为致伤物直接冲击颅盖骨所致，由间接暴力沿脊柱上传造成枕骨大孔区环形凹陷骨折少见。它占颅盖骨折的1/3，多发于颞部，其次为额部和顶部。骨折的尖端常刺破硬膜和损伤脑实质，造成局限性脑挫裂伤和各种颅内血肿及外伤性癫痫。
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