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81.
82.
辽河盆地为中国东部大陆裂谷渤海湾裂谷系的北延部分,是中、新生代发育起来的断陷盆地。 东部凹陷北段是辽河盆地的一部分,也有人将其称为裂谷段,具典型的裂谷盆地的发育特征。经过多条横切构造走向的剖面研究,证实了东部凹陷北段为复式断陷,断陷的走向与盆地走向基本平行。所谓的复式断陷为两个或两个以上的半地堑以某种方式组合而成,在一定时期内,相邻的次一级半地堑各有独立的沉积物供给系统,但当各个次级半地堑充填满以后,相邻的次级地堑具有统一的物源供给系统和水系联通特征,以较大的整体断陷形式继续发育。在控盆断裂一侧的断陷内层序发育较全,而斜坡及边缘地带层序发育不完全,通常缺失低水位体系域或水退体系域。复式断陷不同断陷内的层序,主要受旋回内不同级别幕式构造运动和气候周期性变化的控制,两者的共同作用影响着湖平面的升降和可容空间的变化。由于相邻断陷对物源侵入的阻挡作用,在一定的时期内,各断陷发育独立沉积体系和构造部位的差异,导致了层序地层格架内生储盖层及其组合的发育差异。厚度最大的密集段发育在TST与HST之间,是区域性的生油岩; LST,TST底部,HST顶部、RST通常构成有利储层;密集段也通常成为较好的盖层。在上述因素的作用下,东部凹陷北段复式断陷湖盆中的油气,主要富集在有利构造岩相带的水退体系域、水进体系域和低水位体系域中。层序地层格架内油气藏类型及发育规模存在一定的规律:在缓坡一侧的断陷内,易形成地层超覆型油气藏、地层不整合遮挡油气藏;在陡坡一侧的断陷内,易形成透镜状油气藏、背斜油气藏,起决定作用的是生储盖层的发育状况及其与有利的构造圈闭条件的配置关系。 相似文献
83.
84.
珠江三角洲软土微结构的定量研究 总被引:4,自引:0,他引:4
对用不同长度的PVC管在珠海和广州两地采得的淤泥样柱施于一定荷载,然后在扫描电镜下研究软土受压后在样柱垂深方向上的微结构变化,并将样品的微结构照片扫描,在计算机内进行量化处理。结果表明,样品的孔隙分布分维差随着离施压点距离的增加而逐渐减小,从而得到两者的关系方程。据此,可了解在一定荷载下应力在软土层中向下的衰减趋势。文章还对软土的天然含水量和围压对压缩变形的影响作了初步的讨论。 相似文献
85.
The Upper Permian Sedimentary Facies and Its Role in the Dajing Cu-Sn Deposit, Linxi County, Inner Mongolia, China 总被引:3,自引:1,他引:3
Gongjiong QIN Yosuke KAWACHI Liqing ZHAO Yongzheng WANG Qiang OU 《Resource Geology》2001,51(4):293-305
Abstract: Exhaustive investigations were launched for confirming the upper Permian host rocks of the Dajing Cu-Sn Deposit, probing into the possibility that Dajing is a Sedex type deposit during cosedimentation, complementing the deficiency of previous researches and going further into substantiating the role of the upper Permian strata in the control of ore distribution. After more than two years work, we reclassified the sedimentary facies in the Dajing area and its periphery as shallow fresh water lake and delta. Indicative sedimentary structures, such as ripple marks, rain marks, and mud cracks combined with contemporary fossils, were revealed. Having measured the flow directions, performed chemical comparison, and analyzed various sediments from sourceland in the Dajing area by XRF, we consequently redivided the strata into four sedimentary members, among which P2 l1 and P2 l2 were concluded as significant ore-hosted strata. The upper Permian basin was a lateral rift basin. The water and sediments in the basin are much deeper and thicker in the north than those in the south.
The indicators of special sedimentary facies, such as gravity flow, brine pool and synchronogenic stratiform structure of the ore cannot be found in the Dajing area. There was no growth fault, assemblage of sulfide and sulfate, and no zonation as well.
On the basis of study in this area, taking into account the paleosedimentary environment as capriciously flowing shallow lake, which approximated the state of oxidation, we figured that the paleogeography made it prohibitively difficult to form stratiform sulfide deposits which are prone to form in deoxidized environment. It can be ruled out the possibility that the Dajing deposit is a syngenetic deposit during sedimentation. 相似文献
The indicators of special sedimentary facies, such as gravity flow, brine pool and synchronogenic stratiform structure of the ore cannot be found in the Dajing area. There was no growth fault, assemblage of sulfide and sulfate, and no zonation as well.
On the basis of study in this area, taking into account the paleosedimentary environment as capriciously flowing shallow lake, which approximated the state of oxidation, we figured that the paleogeography made it prohibitively difficult to form stratiform sulfide deposits which are prone to form in deoxidized environment. It can be ruled out the possibility that the Dajing deposit is a syngenetic deposit during sedimentation. 相似文献
86.
在燕山地区东部的滦县等地,太古代至早元古代结晶基底之上发育一套百余米厚的陆源粗碎屑沉积。长期以来,许多研究者将其与蓟县地区长城系近底部的陆相沉积地层对比,认为属于常州沟组。1980年,钱祥麟等经过系统的研究,提出这套地层为晚长城纪大红峪期的超覆沉积。此后,这套粗碎屑沉积的性质及其与盆地整体沉积环境系统的关系。一直未能确定。近年来,笔者为此进行了初步的沉积学研究,结果表明这套粗碎屑沉积与其上的碳酸盐沉积构成了较为典型的 Gilbert 型扇三角洲沉积相。该扇三角洲沉积的确立,为燕山地区中一晚元古代坳拉槽南东缘盆地界线的限定以及早期盆地拉张过程中的沉积充填方式的研究,提供了重要的依据。 相似文献
87.
松辽地区西部斜坡英台地区姚家组二、三段,是在干旱一半干旱、源近流短、东倾陡坡背景下,在洪积扇前,由辫状河入湖形成的辫状河三角洲沉积。可明显区分出狭窄的辫状河三角洲平原,河口坝不太发育的辫状河三角洲前缘和夹浊积砂的辫状河前三角洲三种沉积亚相。辫状河三角洲平原由灰色含砾砂岩,粗、中砂岩,少量细砂岩,粉砂岩夹紫红色泥岩组成。具有明显的正韵律为特征。辫状河三角洲前缘沉积为灰色-绿灰色中、粗砂岩、细砂岩、少量的含砾砂岩,成正韵律或反韵律夹在灰绿色、灰黑色泥质岩中。辫状河前三角洲沉积多为灰绿色、灰黑色泥质岩,可夹少量砂质浊积岩。上述沉积特征明显地区别于正常河流三角洲沉积和扇三角洲沉积。 相似文献
88.
89.
Lower Pleistocene sediments recovered in boreholes from the Aberdeen Ground Formation in the central North Sea indicate that the unit was deposited in a delta front to prodelta/shallow, open shelf marine setting. Possible estuarine and clastic nearshore marine deposits have been identified on the western margin of the basin. The delta front sediments consist of interbedded, structureless to laminated sands and muds with organic debris, ferruginous nodules and common soft sediment deformation structures. Sporadic rippled and graded beds, basal scours to beds and starved ripples suggest periodic wave–current reworking. Prodelta/shelf marine sediments are predominantly argillaceous with only occasional thin sand beds and rare phosphatic bands. One exceptionally thick sand body or submarine channel-fill although this remains uncertain. The estuarine/clastic nearshore marine sediments include coarse channel-lag deposits and rippled and laminated subtidal sands. A rich microfossil assemblage recovered from the prodelta/shelf marine sequence indicates that deposition occurred under fluctuating climatic conditions. 相似文献
90.
Noel Cressie 《Mathematical Geology》1985,17(7):693-702
The relative variogram has been employed as a tool for correcting a simple kind of nonstationarity, namely that in which local variance is proportional to local mean squared. In the past, this has been linked in a vague way to the lognormal distribution, although if {Zt; t D}is strongly stationary and normal over a domain D,then clearly {exp (Zt); t D}will stillbe stationary, but lognormal. The appropriate link is made in this article through a universal transformation principle. More general situations are considered, leading to the use of a scaled variogram. 相似文献