| 1. | Variation features of seismic sequence under tidal effect before m 7 . 0 earthquake lijiang
0级震前地震序列随潮汐作用的变化特征 |
| 2. | The applications of the professional seismic sequence data analysis and processing package easy sequence to earthquake monitoring
地震序列专用处理软件在地震监测中的应用 |
| 3. | Middle - upper ordovician seismic sequences and submarine fan deposits in west tadong uplift , tarim basin , northwest china
塔里木盆地塔东凸起西部中上奥陶统地震层序与海底扇沉积 |
| 4. | On the basis of seismic sequence analysis , sedimentary facies analysis and sedimentary environmental analysis , the main sandstone distribution of each system tract is summarized
在层序划分、沉积环境及沉积相分析的基础上，对主要砂体的展布进行了平面成图。 |
| 5. | We have integrated well - log data with seismic data to study the stratigraphic architecture that utilizes two sequence stratigraphic theories , vail seismic sequence stratigraphy and cross high resolution sequence stratigraphy
综合运用vail和cross的层序地层理论，从测井和地震两方面研究该区层序地层特征。 |
| 6. | A numerical method , rfpa ( superscript 2d ) used in analysis of rock failure process , is applied to study the influence of macroscopic heterogeneity on macroscopic mechanical behavior of rock failure and seismic sequence types
摘要运用岩石破裂过程分析rfpa (上标2d )系统，研究了岩石介质宏观非均匀性（含裂纹）对宏观力学行为和微震序列类型的影响。 |
| 7. | Abstract : seismic facies of jurassic system on east fukang slope in junggar basin are divided and named mainly based on the reliable internal reflection texture and external shape of the seismic sequence unit
文摘:对准噶尔盆地阜东斜坡区侏罗系地层进行了研究，选择了可信度较高的地震反射内部结构和外部形态，辅助地震反射振幅、连续性等参数，对地震相进行了划分命名。 |
| 8. | Through analysis of key - seismic - profiles , it can be divided into 4 seismic sequences from lulehe formation to upper ganchaigou formation , which probably equal to supersequences . in the same time , seismic stratigraphic framework was also established
从骨干地震剖面的层序地层分析可知，区内从路乐河组到上干柴沟组可以划分出4个地震层序，相当于超层序，并建立了地震层序地层格架。 |
| 9. | Basing on the analysis and correlation of the7 wells , 8 seismic sequence boundaries are obtained by logging - seismic correlation , based on seismogram synthesis . more over , they can be traced in the studying region . the synchronic sequence stratigraphic framework is established finally
在单井分析和连井对比的基础上，通过合成记录标定、地震层序的分析，识别出8个三级层序界面，而且完成了全区的主干剖面解释，建立了井震统一的等时层序地层格架。 |
| 10. | Taowan conglomerate was formed with underwater seismism at early cambrian period and consists of shattering sedimentary rock , tsunami rock , seismic turbidite and seismic volcanic rock . the shattering sedimentary rock consists of folded rock , cracked rock and autobreccia . the seismic turbidite is located in the south of luonan ductile shear zone and is called the narrow taowan conglomerate . contrarily the broad taowan conglomerate consists of shattering sedimentary rock , tsunami rock located in the north of the zone . the seismic sequence of shattering sedimentary rock - tsunami rock - seismic turbidite - seismic volcanic rock - normal sedimentary rock was first found in luonan shanxi and is rare among the reported examples about it , so it is a good example and offers power evidences to study how the southern marginal basin of huabei plate transferred to qinling orogenic belt
震浊积岩分布于洛河韧性剪切构造带之南，属传统"陶湾砾岩"范围和涵义，即为狭义陶湾砾岩而广义陶湾砾岩包括分布于洛河韧性剪切构造带之北的震积岩海啸岩及狭义陶湾砾岩。陕西洛南地区首次发现的震积岩海啸岩震浊积岩震火山岩正常背景沉积地震沉积序列之完整在所报导古地震作用沉积序列当中实属罕见，为华北地块南缘造山过程及深入了解古地震作用提供了良好地段和有力证据。 |
