浊流岩

基本解释 (translations)

turbidite

与浊流岩相关的网络例句 [注：此内容来源于网络，仅供参考]

At the same time, the four different genesis types of the sequence interfaces are divided: orogenic erosive sequence unconformity interface, uplift erosive sequence unconformity interface, transgression onlap sequence unconformity interface, exposural sequence unconformity interface; simultaneously the ten concrete mineral showing forms are summarized, i.e. paleo-weathering crust, drossy layer, river rejuvenation surface, paleo-karst surface, slope gravity current erosion surface, intrabasin turbid flow erosion surface, volcanic events surface, lithologic and lithofacies conversion surface, onlap surface and maximium sea flooding surface.

同时归纳出了4种不同的层序界面成因类型：造山侵蚀层序不整合界面、升隆侵蚀层序不整合界面、海侵上超层序不整合界面和暴露层序不整合界面等；同时总结出10种具体的物质表现形式，即：古风化壳、渣状层、河流回春作用面、古喀斯特作用面、斜坡重力流冲刷侵蚀面、盆地内浊流侵蚀面、火山事件作用面、岩性、岩相转换面、上超面和最大海泛面。

The oilbearing analysis of Event Strata indicates that sealevel rising anoxic Event Association is favorable to producing oil, while the sealevel dropping turbidity Event Association may be favorable to reserving oil and gas.

事件地层含油性分析表明，研究区海平面上升-缺氧事件组合是有利的烃源岩，海平面下降-浊流事件组合具有一定的储集意义。

In this area seven microfacies in the Chuangde Fm. red beds can be separated. They are: 1 reddish foraminifera grainstone; 2 reddish microfossils packstone/wackestone; 3 reddish marlstone with microfossils; 4 reddish marlstone; 5 red to variegated floatstone ; 6 reddish shales; 7 reddish radiolarite/ radiolarian chert.In the Yamudok Cuo area, it can be distinguished six microfacies in the redbeds including 1 reddish foraminifera grainstone; 2 reddish microfossils marlstone; 3 reddish shales; 4 yellow-grayish floatstone ; 5 reddish radiolarian chert; 6 reddish chert with radiolaria. The depositional environment of the Chuangde formation can be interpreted from sediments composition, as is deep oceanic basin adjacent to continental slope/rise. The slope/rise setting is indicated by the occurrence of olistoliths and slumped pelagic/hemipelagic limestone, present near the top of the Chuangde Fm.

进一步资料对比研究表明，全球上白垩统海相红层具有以下特征：a上白垩统红层出现在北大西洋、阿尔卑斯、喀尔巴阡、土耳其，向东一直到特提斯喜马拉雅地区和澳大利亚西北角的Exmouth海底高原，横贯整个特提斯和北大西洋；b沉积环境以外陆棚-斜坡和盆地为主，在斜坡环境下多发育有浊流沉积，如Scaglia Rossa和Nietrental组；c有机碳含量普遍很低，0～0.3％之间；d盆地相仅发育红色泥质岩，而斜坡和远洋环境下不仅发育红色页岩，同时还有红色泥灰岩、红色灰岩和红色硅质岩；e北大西洋和地中海地区在Cenomanian-Turonian界线黑色页岩之后不久的Turonian早期就出现红色沉积，而藏南出现在Santonian早期，Exmouth出现在Campanian早期，红层出现似乎有"西早东晚"的趋势。

Studies show that it is a set of turbidity sedimentary under the condition of deep-water environment in rift deep depressing period with the characteristics of multiphase and mutability, The lithology of reservoir is chiefly mid-fine grained conglomerate and lithic mixed sandstone, as well as the gravel-bearing sandstone next. Sand bodies in the plane are controlled by water channel obviously, resulting in NW-oriented banded distribution.

研究表明，大凌河油层是裂谷深陷期深水环境条件下形成的一套浊流沉积物，沉积物具有多期性和突变性，主要岩性以中－细砾岩和岩屑质混合砂岩为主，次为含砾砂岩，砂体在平面上受水道控制明显，呈北西向的条带状展布。

In this area seven microfacies in the Chuangde Fm. red beds can be separated. They are: 1 reddish foraminifera grainstone; 2 reddish microfossils packstone/wackestone; 3 reddish marlstone with microfossils; 4 reddish marlstone; 5 red to variegated floatstone ; 6 reddish shales; 7 reddish radiolarite/ radiolarian chert.In the Yamudok Cuo area, it can be distinguished six microfacies in the redbeds including 1 reddish foraminifera grainstone; 2 reddish microfossils marlstone; 3 reddish shales; 4 yellow-grayish floatstone ; 5 reddish radiolarian chert; 6 reddish chert with radiolaria. The depositional environment of the Chuangde formation can be interpreted from sediments composition, as is deep oceanic basin adjacent to continental slope/rise. The slope/rise setting is indicated by the occurrence of olistoliths and slumped pelagic/hemipelagic limestone, present near the top of the Chuangde Fm.

进一步资料对比研究表明，全球上白垩统海相红层具有以下特征：a上白垩统红层出现在北大西洋、阿尔卑斯、喀尔巴阡、土耳其，向东一直到特提斯喜马拉雅地区和澳大利亚西北角的Exmouth海底高原，横贯整个特提斯和北大西洋；b沉积环境以外陆棚-斜坡和盆地为主，在斜坡环境下多发育有浊流沉积，如Scaglia Rossa和Nietrental组；c有机碳含量普遍很低，0～0.3％之间；d盆地相仅发育红色泥质岩，而斜坡和远洋环境下不仅发育红色页岩，同时还有红色泥灰岩、红色灰岩和红色硅质岩；e北大西洋和地中海地区在Cenomanian-Turonian界线黑色页岩之后不久的Turonian早期就出现红色沉积，而藏南出现在Santonian早期，Exmouth出现在Campanian早期，红层出现似乎有&西早东晚&的趋势。

From late 1940's to 50's, turbidite were widely distinguished in the exploitation of oil and gases as turbidity deposits, and were regarded to be top importance of oil and gases development, warming up turbidity deposits rush all over the world.

从40年代末开始到50年代，在油气勘探中作为浊流沉积的浊积岩被大量辩识出来，并确认了浊积岩在油气开发中具有举足轻重的作用，从而在全球掀起了一股浊流沉积热。

Them etasedimentary rocks are generally turbidite of marine facies in the intetarc basin.

变质沉积岩大致为一套岛弧间海盆地沉积的海相浊流岩。

与浊流岩相关的网络解释 [注：此内容来源于网络，仅供参考]

turbidimetry：浊度测定 浊度测定法 比浊法 测浊法 浑浊度测定

turbidimetrictitration 浊度滴定 | turbidimetry 浊度测定 浊度测定法 比浊法 测浊法 浑浊度测定 | turbidite 浊积岩 浊流层 浊流沉积 浊流岩

turbidite：浊积岩

砾岩的成分、结构、砾石的排列方位以及砾岩体的形态可反映母岩的成分、剥蚀和沉积速度、搬运距离、水流方向等. 浊积岩(turbidite)是浊流沉积形成的各类沉积岩的统称. 常见的有硬砂岩质浊积岩、碎屑灰岩质浊积岩,还有多种浊流成因的岩石类型.

turbidite：浊流岩

隧道谷 tunnel valley | 泥煤 tur | 浊流岩 turbidite

turbidite：浊积岩 浊流层 浊流沉积 浊流岩

turbidimetry 浊度测定 浊度测定法 比浊法 测浊法 浑浊度测定 | turbidite 浊积岩 浊流层 浊流沉积 浊流岩 | turbiditefan 浊积扇

ancient turbidite：古浊流层,古浊积岩

古板块三叉点,古板块三接点 ancient triple junction | 古浊流层,古浊积岩 ancient turbidite | 古水团 ancient water mass