英语翻译次生扇是指形成于扇三角洲前缘的滑积扇.这是一种重力流沉积,主要受陡地形,深水体,强烈构造活动和季节性洪水作用的控制,分布在断陷盆地的陡岸其砂砾岩成分成熟度和结构成熟

英语翻译次生扇是指形成于扇三角洲前缘的滑积扇.这是一种重力流沉积,主要受陡地形,深水体,强烈构造活动和季节性洪水作用的控制,分布在断陷盆地的陡岸其砂砾岩成分成熟度和结构成熟
英语翻译
次生扇是指形成于扇三角洲前缘的滑积扇.这是一种重力流沉积,主要受陡地形,深水体,强烈构造活动和季节性洪水作用的控制,分布在断陷盆地的陡岸其砂砾岩成分成熟度和结构成熟度很低,砂体规模小.一般地说,在扇三角洲前缘,只要有同生沉积断层存在,就有可能形成滑塌扇.粗碎屑主要来自陡岸侧的扇三角洲,滑塌构造极为发育,夹有少量高密度浊流沉积及其鲍马序列为其特征.以正粒序层理和块状层理为其显著特征.其次为包卷层理,平行层理,板状交错层理,小型交错层理,变形层理和不规则交错层理,反映了以重力流为主的沉积构造和韵律特征.
次生扇的形成有主客观两类因素的控制.主观方面,扇三角洲前积层坡地一般较大,容易产生滑塌.客观因素有很多,如地震、波浪等作用都会导致扇三角洲前缘滑塌.对于陆相小型湖盆来说,地震活动可能是最主要的诱发因素.次生扇油气藏岩性较扇三角洲细,深入湖中心泥岩,被泥岩包围,并常有断层与之配合成藏,而且靠近烃源岩,所以次生扇是很好的储集体.
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英语翻译次生扇是指形成于扇三角洲前缘的滑积扇.这是一种重力流沉积,主要受陡地形,深水体,强烈构造活动和季节性洪水作用的控制,分布在断陷盆地的陡岸其砂砾岩成分成熟度和结构成熟
fanzian
好厉害的复制好手……机器翻译,错误的太多了
从第一句话就看出你翻译的不对……

Secondary fan is a fan in front of the Delta slide fan. This is a gravity-flow deposits, mainly by Doude-Sham body, strong tectonic activity and the role of the seasonal flood control, located in the ...

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Secondary fan is a fan in front of the Delta slide fan. This is a gravity-flow deposits, mainly by Doude-Sham body, strong tectonic activity and the role of the seasonal flood control, located in the rift basin steep shore glutenite its composition and maturity structure of maturity is very low, sand A small scale. Generally speaking, the fan delta front, as long as the existence of fault with the deposition of Health, it is possible to form slump fan. Crude debris from the steep shore-side fan delta, the very structure of slump, clip a small amount of high-density turbidity Baoma sedimentary sequence and its features. To sequence tablets are massive bedding and bedding for significant feature. This was followed by bedding package volumes, parallel bedding, tabular staggered bedding, small staggered bedding, bedding and irregular deformation staggered bedding, reflecting the gravity flow mainly to the sedimentary structure and rhythmic features.
The formation of a secondary fan both subjective and objective factors of control. Subjective, the fan delta before the general slope of the larger plot, easy to have a slump. There are many objective factors, such as earthquakes, waves, and so the role would lead to fan delta front slump. For continental small lake, seismic activity may be the most important factors induced. Secondary fan reservoir lithology more fan delta small, in-depth Lake Centre mudstone, shale was surrounded, and often meet with the fault-forming, and near the source rocks, the secondary fan is a very good reservoir.

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翻译过后: 下文,谢谢你的分.
The secondary fan is refers to forms accumulates the fan slippery in the fan delta front. This is one kind of mass flow deposition, mainly the steep terrain, the deep water body, ...

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翻译过后: 下文,谢谢你的分.
The secondary fan is refers to forms accumulates the fan slippery in the fan delta front. This is one kind of mass flow deposition, mainly the steep terrain, the deep water body, intensely is constructed active and the seasonal flood function control, distributes is breaking falls the basin steep coast its granulated substance conglomerate ingredient maturity and the structure maturity is very low, the granulated substance body scale is small. Generally speaking, in fan delta front, so long as has the syngenesis to deposit the fault existence, has the possibility to form collapses slippery the fan. The thick detritus mainly comes from the steep coast side the fan delta, collapses the structure to grow extremely slippery, clamps has the few high density turbidite and the Bao horse sequence for its characteristic. Take the grain of foreword bedding and the massive bedding as its dominant character. Next is the involution bedding, the parallel bedding, the plate-type cross stratification, the small cross stratification, the deformed bedding and the anomalous cross stratification, have reflected by the mass flow sedimentary structure and the rhythm characteristic primarily. the secondary fan's formation has the subjective and objective two kind of factor controls. The subjective aspect, the fan delta foreset bed land on slopes is generally big, easy to produce collapses slippery. The objective factor has many, like functions and so on earthquake, wave can cause the fan delta front to collapse slippery. Regarding the land facies small lake basin, the seismic activity is possibly the most main suggestion factor. The secondary fan oil gas pool lithological character compares the fan delta to be thin, the thorough lake center mudstone, by mudstone surrounding, and the common fault coordinates with it Tibet, moreover approaches the hydrocarbon source rock, therefore the secondary fan is the very good accumulation body.

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