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- secondary fault basin 次级断裂盆地
- Fuxin basin is a J3-K1 fault basin. 阜新盆地是中燕山期(J3-K1)断陷盆地。
- Anning Basin is a terringenous fault basin developed in Mesozoic Era. 云南安宁盆地为中生代陆相断陷盆地。
- Liaohe Basin is a fault basin of rift valley type formed in Cenozoic Era. 辽河盆地是一新生代断陷盆地;盆地内天然气资源丰富;天然气成因复杂.
- NNE Kuerbin crustal fault and its secondary fault anr the important conditions for ore forming. NNE向库尔滨壳断裂及其次级断裂为成矿的重要地质条件。
- Gaobei Syncline is major fold,a lot of secondary fault later period Indo-China play a comtrol role to mine area mainly formed three decollement fault. 对矿区起控制作用的断层是滑覆断层。印支晚期主要形成三条滑覆断层;燕山早期形成高陂向斜;燕山中晚期形成南北边界逆断层,形成了高陂向斜南高北低格局。
- Yingen-Ejinaqi Basin is a Mesozoic and Cenozoic lacustrine fault basin, and pre-Mesozoic constitutes its basement. 银根-额济纳旗盆地是中新生界陆相盆地,前中生界构成盆地基底。
- The northeast Ehen secondary fault depression, maoxi fault-nose and maonan slope should be favorable places for prospecting in the near future. 提出了额很洼陷东北部和毛西断鼻构造以及毛南斜坡,是近期首选的有利勘探目标区带。
- The Yitong Graben is a Tertiary petroliferous strike-slip fault basin developed on the Hercynian fold basement. 伊通地堑是一个主体在海西期褶皱基底上发育起来的第三纪含油气走滑断陷盆地。
- Abstract: The overthrust had developed on the margin of the fault basin in the west of Liaoxi sag. 中文摘要: 辽西坳陷中的断陷盆地边缘逆冲断层发育。
- Hydrocarbon accumulation in FL strike-slip faulted basin. FL走滑型断陷油气富集特征
- Dong-pu Sag is a fault basin in palaeogene, with overlying depressed-type sediments in Neogene. 东濮凹陷在古近纪为断陷盆地,新近纪为坳陷沉积。
- The intermediate-acid extrusive rocks formed from Paleozoic to Mesozoic or Cenozoic era are the main sections of the sediment profiles in fault basin. 已被勘探的中酸性喷出岩的地质年代从古生代到中生代和新生代。
- The Daqingshan Mountains and its adjacent Huhehot fault basin, Nei Monggol, are the ideal area to study denudation and uplift. 内蒙古大青山及其毗邻的呼和浩特断陷盆地是研究剥蚀和地壳均衡隆起的理想地区。
- There are the trends that the evolution of faults is from a combination of complex and secondary faults to an simple,successive and primary fault. 断裂的空间分布为多重分形结构,断裂的演化有从复杂几何结构的次级断裂组合向单一连续的大断裂过渡而分维值逐渐减小的趋势;
- Lying in the east of Heilongjiang province, Yishu graben is a Cenozoic fault basin comprising two large second-class structural units, i. 依舒地堑位于黑龙江省东部,为一新生代断陷盆地,汤原断陷和方正断陷为其两个面积较大的二级构造单元。
- According to the study of mantle plume for ten years,it is concluded that sub-mantle plume is strongly uplifting under fault basin of North China. 笔者依据近十余年华北地幔亚热柱的研究认为,华北断陷区之下为一强烈上隆的地幔亚热柱。
- The secondary faults developed in the thrust block at the inflection point of the nappe structural plane are the principal ore-hosting structure. 矿化带和矿体的形态、产状、分布和规模均严格受赋矿构造的控制。
- Characteristics of alluvial fans at margins of faulted basin are researched. 对断陷盆地边缘冲积扇发育规律进行了探讨;
- The antimony deposit occurs on the south side of the major Muzitage sliding fault.The mineralization belt is controlled by secondary faults striking NEE and EW. 锑矿产于木孜塔格大型走滑断裂南侧,矿化带受NEE向及EW向次级断裂控制,矿体形态相对复杂,多为似层状、脉状、网脉状、囊状等。