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Because of the stratigraphic conditions of multi-lithologies and thin-bed association, unstability of lithofacies in the vertical and lateral direction, and the particalar conditions of seissmic geology in Inland Basins, Western China, a stratigraphic model of sedimentary facies in which there are many theoretical reflecting seismic interface does not completely display on the seismic section, especially the some the most important stratigraphic information such as toplap, onlap, progradation, erosional truncation and fill of channal, divergent, shingled, ect.

本文在研究了9类沉积相及相组合地层模型的地震模拟记录后证明:现今流行的在地震剖面上划分地震相进而应用国外海相地层反射模式再转换为沉积相这一所谓&相面&方法完全不适用于西部陆相盆地沉积相地层模型的特点,作者首次开辟了用速度参数,合成地震记录、二维地层模型技术研究西部盆地地下沉积相的新途经。

The lining is an unsealed copper ring; the section of the lining inner cavity is a ladder cavity, the bottom is equipped with an edge shaped via enclosing a crucible; the heating coil is silverly welded in the arc groove of the cylindrical surface of the lining, and the upper of the lining winds a few turns coil around the center of the crucible; the two ends of the composite induction heating device are accessed to a high frequency induction power respectively.

内衬(11)为未封闭铜圆环;内衬内腔的剖面为梯形空腔,底部有装入坩埚(4)的刃形通孔(12);加热线圈(10)银焊在内衬外圆表面的弧形凹槽中,并在内衬(11)上方以坩埚(4)为中心绕制数匝线圈;将复合感应加热装置(5)的两端分别接入高频感应电源(9)。

This section of eroded sedimentary rock on Elgol Beach on the Island of Skye, Scotland, mimics bone.

这个剖面是侵蚀水成岩在Elgol海滩位于苏格兰的斯开岛,模仿的骨骼。

The most dramatic surface karst landforms cover an area of 40 km2, exposed limestone surfaces have been dissected by the formation of enormous karren with solution runnels, deepening of the karren and solutional opening of joint fissures has left remnant pinnacles of various shapes, which are described as stone forest.

地表石海分布面积达40余平方千米,是研究地表岩溶的绝好场所。形成地表石海的岩层是由距今约2.9亿年的海相碳酸盐沉积而成。典型的地质剖面以及地层中保存的特殊沉积构造与丰富的古生物化石,全面反映了该地区沉积环境和构造演化的历史。

Grainstones are the main part of the section, among which the oolites, intraclast limestones and most bioclast limestones are cemented by sparry calcite.

颗粒灰岩在剖面中占绝大多数,其中,鮞粒灰岩、內碎屑灰岩和多数生物碎屑灰岩均为亮晶方解石胶结。

According to a detailed structural analysis and stratigraphic sections,the stratal sequences of the Huade Group have been reconstructed;the group may be subdivided in ascending order into the Maohuqing Formation,Gejiaying Formation and Sanxiatian Formation.

依据详细的构造解析和地层剖面研究,重新建立了化德群的地层层序,从老到新划分为毛忽庆组,戈家营组和三夏天组。

On the basis of field investigation and seismic section interpretation, the Kalpin thrust belt has the following structural deformation characteristics: the thrust belt occurs in Paleozoic strata; the major detachment fault occurs in a Middle Cambrian gypsum-salt layer; the thrust sheets are imbricate; various thrust fronts are subaerially exposed; fault propagation folding and piggyback thrusting are found; and the thrust belt formed during the Pliocene-Holocene.

根据野外实际考察和地震剖面解释,总结了该冲断带的构造变形特征:发育于古生界、以寒武系膏盐层为主滑脱层、叠瓦状冲断、暴露式冲断前锋、断层传播褶皱、前展式冲断、形成于上新世—第四纪。

The CMP record was processed by conventional flow, and stacked and deviated sections were obtained, the response characters of pinchout sand bodies are analyzed, the seismic attributes such as root-mean-square amplitude and its variation are determined as sensitivety parameters of oil and gas reservoirs, a concept seismic-geologic model of sublacustrine fan reservoir is established, by which the multiplicity and limitation are reduced for prediction, a basis is provided for seismic interpretation.

对共炮点记录进行常规处理,得到叠加和偏移剖面。分析尖灭砂体的地震响应特征,确定了均方根振幅和振幅变化率等地震属性为含油气储层敏感参数。并建立了湖底扇储集体概念化地震地质模型,减少了预测的多解性和局限性,可为地震解释提供科学依据。

Secondly, through the identification of facies marks and the analysis of sedimentary facies cross sections, alluvial fan, river, fan delta, delta, lake, sublacustrine fan and tempestite sediment environment have been developed in West Chaidam Basin.

其次,通过对相标志的识别和对反映沉积相纵向演化的基干剖面的分析,总结出研究区发育了冲积扇相、河流相、扇三角洲相、三角洲相、湖泊相、湖底扇相以及风暴沉积等沉积相类型。

The Es formation was divided into seven third order sequences based on the seismic, drilling and logging data, and plans deposition system plane distribution maps of different time were plotted by dominance phase principle. The lower Es4 is flood-overlake facies mainly; the upper Es4 is meandering stream and braided river delta deposition above the shore shallow lake background; in the Es3 period, the south mainly developed braided river, meandering stream delta, the northeast area main developed meandering stream delta, the middle area mainly developed semi-deep lakean d deep lake sediments. From lower Es3 to upper Es3, the delta scale gradually increased and the depositional area gradually moved to the east and the southeast; the Es2 period was dominated by shore-shallow lake sediments and widely developed braided river delta and delta deposits; the Es1 period was dominated by shore-shallow lake shoal deposits, and in the south developed meandering stream and braided river delta deposits.The lothological traps of the Shahejie group are mainly fluxoturbidite and stratum lateral pinch-out, and its formation and the distribution of the lothological trap were controlled mainly by the basin structure characteristic, palaeogeomorphology and tectonic activity and so on. It had a beneficial geological condition to develope sublacustrine slump turbidite fans in Jishan, Jiangjiadian and Wawu.

利用地震、钻井、测井等资料,将古近系沙河街组划分出7个三级层序,通过剖面沉积学分析,以优势相原则绘制不同时期各亚段沉积体系平面分布图:沙四下总体以洪水-漫湖沉积为特征,沙四上沉积时期是在滨浅湖背景之上发育了曲流河三角洲和辫状河三角洲沉积;沙三段沉积时期南部主要发育辫状河、曲流河三角洲,西北部地区发育曲流河三角洲,中部地区主要为深湖—半深湖沉积;由沙三下至沙三上,西北部三角洲规模逐渐增大,沉积范围逐渐向东、东南方向推进;沙二段沉积时期为滨浅湖沉积,在背景之上广泛发育了辫状河三角洲和三角洲沉积;沙一段以滨浅湖滩坝沉积为特征,南部发育了曲流河三角洲和辫状河三角洲沉积;沉积地层中的岩性圈闭以滑塌浊积岩岩性圈闭和地层侧向尖灭型岩性圈闭为主,其形成和分布主要受盆地结构、沉积古地貌和构造活动强度等因素控制,北部基山、南部江家店和瓦屋具有发育滑塌浊积扇的良好地质条件。

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