diapir

diapir

1. Keywords DF1-1 diapir;fault system;gas accumulation;gas migration.;

1底辟;断裂系统;天然气成藏;天然气运聚;

2. falling diapir

下降盐刺穿

3. immature diapir

不完全底辟构造

4. The Elementary Research of Gas Hydrate Associated with Mud Diapir Structure in the East China Sea

东海与泥底辟构造有关的天然气水合物初探

5. There are 3 types of reservoir for the continuing subsidence type basin, there are diapir reservoir, fault reservior, drape reservoir, and the source rock is apart from the reservoir,they are contact by fault;

以沉降为主要趋势的盆地的油气藏有底辟构造油气藏、断层油气藏、披覆构造油气藏，其烃源岩与油藏在空间上是分离的，并通过断层相连；

6. cold diapir

冷底辟

7. SEISMIC INFORMATION OF COLD DIAPIR AND HOT DIAPIR

冷底辟与热底辟地震信息

8. Primarily Analyzing the Diapir Structures of Lower Palaeozoic in the Transition Belt between the Southern and Central Parts of Sichuan

初析川中川南过渡带下古生界之穿刺构造

9. Magmatic Diapir of Fangshan Pluton in the Western Hills, Beijing and Its Geological Significance

北京西山房山岩体岩浆底辟构造及其地质意义

10. The main types of subtle reservoirs in the north of South China Sea are lithologic reservoir,stratigraphic reservoir,burial hill reservoir and diapir reservoir.

南海北部隐蔽油气藏主要类型以岩性、地层、潜山和底辟为主,而主要发育于盆底扇、斜坡扇、陆架边缘三角洲和碳酸盐岩等沉积体系内。

11. Negative coefficients occur where there is a downward decrease in velocity and density: for example, at the top of an over pressured shale diapir

只有当速度和密度向下减少时，例如在超压页岩穿刺体的顶部，反射系数才会出现负值。

12. For the exploration of gas hydrates,it is of great significance to study such geological structures as mud diapir and mud volcano.

在天然气水合物勘探中,海底的泥底辟和泥火山构造是重要的研究对象。

13. Gas hydrates were formed due to the availability of free gas within the diapir structures from the bottom of gas hydrate stability zone up to the sea floor.

在底辟构造中，由于游离气体的向上迁移，在整个水合物稳定域中从下到上，直至海底都可能形成水合物，从而使我们有机会使用重力采样器这样的设备也能采获天然气水合物样品。

14. In the high-resolution seismic profile,to directly identify the diapir is often difficult due to much similarity between diapir and the invasion of igneous rock,thus leading to multi-resolution.

在高分辨率地震剖面解释中,直接识别泥底辟构造存在一定困难,主要因为泥底辟构造和火成岩侵入体在形态上十分相似,容易造成解释的多解性。

15. 1.In the high-resolution seismic profile, to directly identify the diapir is often difficult due to much similarity between diapir and the invasion of igneous rock, thus leading to multi-resolution.

在高分辨率地震剖面解释中，直接识别泥底辟构造存在一定困难，主要因为泥底辟构造和火成岩侵入体在形态上十分相似，容易造成解释的多解性。

16. mantle diapir

地幔底辟构造

17. Keywords gas hydrate;mud diapir;seismic attribute;prestack full waveform inversion;Okinawa Trough;

天然气水合物;泥底辟;地震属性;叠前全波形反演;冲绳海槽;

18. Keywords BSR;gas hydrate;slumping block;mud diapir;thrust nappe structure;accretionary wedge;Hengchun ridge;

天然气水合物;滑塌体;泥底辟;叠瓦状逆冲推覆构造;增生楔;恒春海脊;

19. magma diapir

岩浆底辟

20. Besides,the mechanism and geologic setting of fluid diapir are analyzed,on the basis of the theory of fluid fracturing.

并在综合分析国内外流力破裂研究成果的基础上，论述了流体底辟形成的机制和地质背景。

21. diapir structure

底辟构造

22. The relationships between diapir structure and gas hydrate mineralization

底辟构造与天然气水合物的成矿关系

23. diapir structure belt

底辟构造带

24. diapir core

底辟核

25. plis diapir

底辟褶皱

26. Abnormally high CO2 content is unigue only in shale diapirs.And the higher evolution of diapir is , the higher CO2 content would be.

异常高的CO_2为泥拱带所独有,并且泥拱演化序列越高泥拱帽CO_2含量越高,断块越小CO_2含量越高,越是靠近断层CO_2含量越高。

27. diapir dome

挤入穹丘

28. diapir fold

挤入褶皱

29. For the exploration of gas hydrates, it is of great significance to study such geological structures as mud diapir and mud volcano.

摘要在天然气水合物勘探中，海底的泥底辟和泥火山构造是重要的研究对象。

30. Keywords Songliao Basin;deep seated structures;seismic exploration;tenacious shacer zone;mantle thermal diapir;

松辽盆地;深部构造;深部地震勘探;韧性剪切带;地幔热底劈体;

31. According to mixed ratio of mudrock,fluid diapir structure can be divided into four types:fracture zone,chaotic fracture zone,mixed sandstone-mudrock zone (or mudlump) and mud volcano.

根据流体底辟破碎带中泥质混入程度，将它分为断裂破裂带、混杂破裂带、混合岩带和泥火山4种类型；

32. Mud-fluid diapir

泥-流体底辟

33. mud diapir

泥底辟

34. diapir origin

泥底辟成因

35. mud diapir structure

泥底辟构造

36. Keywords mud diapir structure;mechanism of geodynamics;experiment of high T and P;

泥底辟构造;动力学成因机制;高温高压实验;

37. heat flow in the diapir belt

泥底辟热流体

38. Keywords thermal fluid in the mud diapir;heat field character of a basin;migration and accumulation characteristics of natural gas;controlling factor analysis;the Yinggehai Basin;

泥底辟热流体;盆地热场特征;天然气运聚特点;控制因素分析;莺歌海盆地;

39. Keywords mud diapir: structure;mechanism;Yinggehai Basin;

泥拱;结构;形成机制;莺歌海盆地;

40. Mud diapir is an important geologic phenomenon related to gas accumulation in Yinggehai Basin.

泥拱是莺歌海盆地的重要地质现象,它与油气聚集有密切关系。

41. Mud diapir is consisted of reservior, vent and cap.

泥拱由泥拱房、泥拱颈和泥拱帽组成。

42. Keywords mud volcano;mud diapir structure;gas hydrate;East China Sea;

泥火山;泥底辟构造;天然气水合物;东海;

43. Keywords Bohai Bay Wenliu seruceure salt structure reactive diapir scaled physical modeling structural geology;

渤海湾;文留构造;盐构造运动;次动盐刺穿;物理模拟;构造地质学;

44. THE PALEOKARST GENESIS OF THE DIAPIR OF KUNYANG GROUP IN CENTRAL YUNNAN

滇中昆阳群刺穿体构造的古岩溶成因

45. Keywords thermodynamic effection;differential gravity action;diapir;geometric configuration;

热动力效应;差异重力作用;刺穿;几何形态;

46. Keywords Qiongdongnan basin;tectonic restoration;gas hydrate;mud diapir structure;

琼东南盆地;构造复原;天然气水合物;泥底辟构造;

47. Keywords geotemperature field;mud-fluid diapir;heat flow;migration and accumulation of natural gas;the Yinggehai basin.;

盆地地热场;泥-流体底辟;热流体;天然气运聚;莺歌海盆地;

48. Faults and diapir develop widely and influence the distribution of gas hydrate.

盆地广泛发育断裂、底辟构造，影响着水合物的分布。

49. salt diapir

盐丘 盐刺穿 底辟盐丘

50. Salt diapir screened hydrocarbon reservoir

盐丘遮挡油气藏

51. Diapir of gypsum-salt layers

膏盐层底辟

52. Keywords Yinggehai basin;diapir structure belt;fluid fracture;hot fluids acitvity;migration-accumulation madel;

莺歌海盆地;底辟构造;流体压裂;热流体活动;运聚模式;

53. Keywords Yinggehai basin;mud-fluid diapir;disequilibrium compaction;thermal evolution;episodic injection;

莺歌海盆地;泥-流体底辟;不均衡压实;热作用;幕式充注;

54. Keywords Yinggehai Basin;mud diapir structure;modelling structural experiment;mecha-nism.;

莺歌海盆地;泥底辟构造;构造模拟实验;成因机制;

55. There are extraordinary active thermal fluids in the mud diapir zone of central depression in Yinggehai basin.

莺歌海盆地中央坳陷泥底辟带是一个热流体非常活跃的地区。

56. The Exploration Outlook of Natural Gas under High Temperature and High Pressure in Medium-Deep Layer in the Shale Diapir Belt of the Yinggehai Basin

莺歌海盆地底辟带中深层高温超压领域天然气勘探前景分析

57. The Yinggehai basin is characterized by high thermal gradients and overpressure.The diapir structure zone contains rich resources of oil and gas.

莺歌海盆地是中国近海最重要的天然气探区之一,具有超高温及异常高压的独特地质条件,中央坳陷形成了众多巨型泥底辟构造。

58. GENETIC MECHANISMS OF MUD-FLUID DIAPIR IN YINGGEHAI BASIN AND HYDROCARBON ACCUMULATION

莺歌海盆地泥-流体底辟构造成因机制与天然气运聚

59. Both shallow and deep gas plays are present in the mud diapir belt.

莺歌海盆地泥底辟带存在浅层和中深层2套含气组合。

60. The middle-deep beds are very important new hydrocarbon exploration area in the Yinggehai Basin where there are some mud diapir belts with abnormal high temperature and pressure.

莺歌海盆地泥底辟带异常高温高压的中深层目的层是该盆地新的油气勘探领域。

61. GEOPHYSICAL CHARACTERS AND ORIGIN OF THE THERMAL FLUIDS IN CHANGNAN BLOCK OF MUD DIAPIR ZONE IN YINGGEHAI BASIN

莺歌海盆地泥底辟带昌南区热流体活动的地球物理特征及成因

62. The mud diapir structure in Yinggehai Basin,South Chian Sea,was been formed and evoluted mainly by thermodynamic actions.

莺歌海盆地泥底辟构造主要是在热动力作用下形成和演化的,包括热传导和热对流作用。

63. As the seabed erosion rate decreases, the diapir shrinks gradually and disappears finally due to the erosion.

软弱层变形及刺穿对海洋工程设施危害极大。

64. Aiming at exploring the medium-deep layers of mud diapir belt in the Yinggehai Basin, CNOOC drilled two wells at the end of 20th century.

针对莺歌海盆地底辟带中深层,中国海洋石油总公司在20世纪末批准并上钻了两口探井。

65. The interpretation of a typical sub-bottom profile reveals that the diapir of the Yellow River delta resulted from the interior deformation of soft prodelta layers at the delta front.

高分辨率黄河三角洲典型的地震地层和解释地层剖面、浅地层剖面和钻孔资料联合解释表明,海底刺穿的发源层来自于河口沙坝下部的前三角洲相软弱层变形。

66. Keywords the characteristics of high geotemperature and superpressure;heat flow in the diapir belt;factors controlling gas reservoir;the Yinggehai basin;

高温高压;泥底辟热流体;成藏控制因素;莺歌海盆地;

67. diapir hot fluid activiw

高温高压潜能

68. After the river channel shifted, the discharging center of pressure was generated from the seabed erosion, on which the diapir came into being.

黄河口摆动后，海底快速冲刷，在最大冲刷中心也是最大压力释放中心刺穿体形成，随着海洋侵蚀速率减缓，刺穿作用将逐渐减弱，最终将被冲刷消亡。