- 更多网络例句与腐泥岩相关的网络例句 [注：此内容来源于网络，仅供参考]
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Results show that obduction and napper were main tectonic movements in late Indosinian-early Yanshan period of Lower Yangtze Region, and most areas were elevated and denudated. Source rocks of lower-Paleozoic in some areas did not deep bury renewedly, and remain the Indosinian thermal evolution state. Therefore the high maturity sapropelic organic matter of lower-Paleozoic has still possessed hydrocarbon generation potential.
研究结果表明，晚印支-早燕山期，下扬子区的构造运动以逆冲推覆为主，大部分地区遭到抬升剥蚀，部分地区下古生界烃源岩抬升后晚期没有再度深埋，保留了印支期的热演化状况，因此下古生界高成熟腐泥型烃源岩现今仍具有一定的生烃潜力。
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The result shows that oil and gas from Xujiahe group mainly comes from autogenic coal source rock,and bind is main.Genetics of natural gas is mainly mature humic mothermaterial,small condensate oil and crude oil is m... \r\n
指出须家河组油气主要来自须家河组自身的煤系烃源岩，并以煤系泥岩贡献为主；天然气以成熟腐殖型母质成因为主，少量的凝析油和原油来自其中的混合型有机质，不具备典型煤成油特征。
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The paper adopts some methods such as gas composition, carbon isotope, systematical analyzing and testing of reservoir bitumen biomarker from high evolutional natural gas and quantitative calculation of mixed gas, illustrates that natural gas from the section Ⅱ of Jialingjiang formation is mainly attributed to sapropel type organic matter gas of Permian, comes from carbonatite hydrocarbon rocks Permian which most of them are overmature, its main gas source has nothing to do with carbonatite hydrocarbon rocks of Jialingjiang formation themselves, presents in geochemistry characteristics of oil type cracked gas.
摘要通过对川中－川南过渡带西部的磨溪－潼南地区嘉二段天然气组成、碳同位素组成、高演化天然气储层沥青生物标志化合物的系统分析测试和混合成因气的定量估算，阐明了该区嘉二段天然气主要属于二叠系腐泥型有机质成因气，来源于二叠系过成熟为主的碳酸盐岩烃源，主力气源与嘉陵江组自身的碳酸盐岩烃源无关，并具有油型裂解气的地球化学特征。
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In a view of the theory of the traditional oil and gas formation it is considered that the oil and gas resources buried in sedimentary basins are generated by OM in source rocks during thermal evolution and marine, lacustrine sapropel and humic-sapropel OM is the mater of the formation of considerable oil and gas but coal-measure strata is relatively bad source rocks, being considered that they can not generate significant amounts of oil and gas.
传统的石油天然气成因理论认为蕴藏于沉积盆地的油气资源是由烃源岩中的有机母质在热演化过程中形成的，而且是海相或者湖相腐泥型和腐泥－腐殖混合型的有机质有利于形成大量的石油和天然气，而煤系地层相对是较差的烃源，认为这种烃源岩不能形成大量的油气。
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Microorganism not only is a kind of hydrocarbon- generating components participating in sedimentary organic matter formation directly, but also can impel "humic" organic matter to transform into "sapropel" organic matter, so as to improve organic type and raise hydrocarbon-generating potential of source rocks.
微生物不仅本身能做为生烃成分，直接参与沉积有机质形成，而且还可使&腐殖型&有机质转向&腐泥化&，改善有机质类型，提高源岩的生烃潜力。
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The mineralogical and geochemical research on grey-brown laminatedmud stone, oil shale of Shahejie Formation Member 1 of Gulan Subsag found that the content of sapropel was all over 97% and the content of organic matter and chloroform bituments "A" was over 1% and 0.1% respectively in 35 samples. The organic matter belonged to type I and reached the standard of good source rocks.
对孤南洼陷沙一段灰褐色纹层泥岩和油页岩、深灰色油泥岩、深灰色泥岩、灰质泥岩样品进行岩矿及地球化学分析，35块样品的腐泥组含量全部大于97％，表明生烃母质主要为藻类，为Ⅰ型有机质，所有样品的有机碳含量都＞1，氯仿沥青&A&含量＞0.1，全部达到&好烃源岩&标准，是该地区的一套优质烃源岩。
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Based on the comparison of oil-rich and gas-rich sag s in the Bohai Bay basin,two main controlling factors of gas reservoir-forming are summarized: gas-rich sag s have source rock of partial humic or high maturation sapropel type;thick abnormal pressure mudstone in lower Tertiary is the cap,or "quilt".
对比研究渤海海域及周边陆地油区主要气田特征，发现渤海海域天然气成藏的主控因素有两点：存在相对富气凹陷，气源岩为偏腐殖型或高成熟腐泥型；富气凹陷的古近系发育高压异常厚层泥岩封盖层。
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Considing the geological setting of the source rocks and the secondary hydrocarbon generation factors of primary maturity, major hydrocarbon generation stage and the organic matter type,two series of samples of humic and sapropelic organic matter had been selected.
根据烃源岩发育的地质背景，综合考虑二次生烃的原始成熟度、主要生烃阶段、有机质类型等因素，用高压釜和热解生烃模拟实验完成人工模拟和自然演化系列的两组样品腐植型和腐泥型共16个。
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Dark mudstones were developed in the maximum lake flooding period of Chang 7,which are the main source rocks.
延长组长7段最大湖泛期发育一套暗色泥岩，干酪根类型为腐植-腐泥型，是盆地主要生油岩。
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On the basis of oil source correlation , the paper studied the organic microscopic component of the immature hydrocarbon source rock in santanghu basin.
本文在油源对比的基础上，对三塘湖盆地低熟源岩有机显微组分进行研究，认为盆地主力源岩芦草沟组主要生烃显微组份为腐泥无定型组。
- 更多网络解释与腐泥岩相关的网络解释 [注：此内容来源于网络，仅供参考]
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sapropelic groundmass：腐泥基质
sapropelic coal 腐泥煤 | sapropelic groundmass 腐泥基质 | sapropelite 腐泥岩
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kerogen sapropelite：干酪根腐泥岩
kerogen rock 干酪根岩 | kerogen sapropelite 干酪根腐泥岩 | kerogen shale 干酪根页岩
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saprolite：腐泥岩、腐泥土
Sandy soil 砂土壤 | Saprolite 腐泥岩、腐泥土 | Saturated unit weight 和位重
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saprolite; saprolith; sapropelic rock：腐泥岩
腐植软泥 saprogeneous ooze | 腐泥岩 saprolite; saprolith; sapropelic rock | 腐生风化 saprolitic weathering
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sapropelic rock：腐泥岩
腐泥煤 sapropel-peat | 腐泥岩 sapropelic rock | 腐泥岩系 sapropelite series
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sapropelic clay：腐泥黏土
"腐泥的","sapropelic" | "腐泥黏土","sapropelic clay" | "腐泥岩","sapropelic rock"
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sapropelite：腐泥岩
sapropelic coal 腐泥煤 | sapropelite 腐泥岩 | saturate 饱和
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sapropelite：腐泥岩离心喷雾干燥机
sapropelic coal 腐泥煤 | sapropelite 腐泥岩离心喷雾干燥机 | saturate 饱和
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kerogenetic sapropelite：干酪根腐泥岩
kerogen 干酪根 | kerogenetic sapropelite 干酪根腐泥岩 | kerogenic 干酪根的
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sapropelite series：腐泥岩系
腐泥岩 sapropelic rock | 腐泥岩系 sapropelite series | 腐生植物 saprophyte