熱演化 的英文怎麼說
中文拼音 [rèyǎnhuà]
熱演化
英文
thermal evolution-
In this paper, thermal evolution history of organic matter of the source rocks and hydrocarbon generation history have been researched by tti method, hydrocarbon migration direction and migration times were probed combining with the area structure development feature ; distribution pattern of the main reservoir intervals on lateral and longitudinal have been predicted by researching on development feature and control factors of the reservoir intervals, the actions of reservoir conditions in hydrocarbon accumulation and bearing also were probed combining with pore evolution feature ; the micro - pore feature of regional cap and direct seal in carboniferous - lower triassic in this area have been determined with micro - capillary pressure curve and intrusive mercury curve ; the prospecting districts have been pointed out combining with the hydro - geologic feature, the potential reservoirs were classified according to trap types in this area, the author attempt to evaluate on the hydrocarbon - bearing condition in the str ata of carboniferous ~ lower triassic from hydrocarbon generation and migration reservoir condition, reserved condition etc, and predict the reservoir types and hydrocarbon - bearing patterns combining with the structure evolution. based on above, the author point out that the central block of chenghu - tuditang synclinorium and the southern block of dangyang synclinorium are the advantageous regions for exploration
本文用tti方法研究了烴源巖有機質的熱演化史和油氣生成史，並結合區內構造發育特徵，探討油氣在區域上的運移方向和在時間上的運移期次；通過對儲集層段的發育特徵和控制因素的研究，預測了本區主要的儲集層段在橫向上和縱向上的分佈規律，並結合孔隙演化特徵，探討儲集條件在油氣聚集成藏中的作用；利用微毛細管壓力曲線法和壓汞法，對石炭系?下三疊統的區域蓋層和直接蓋層的微孔隙特徵進行了定量評價，並結合水文地質分佈特徵，指出有利於油氣保存的地區；根據區內存在的各種圈閉類型，對可能存在的油氣藏進行了分類，並試圖從油氣的生成與運移、儲集條件、保存條件等方面，動態地綜合評價石炭系?下三疊統油氣成藏條件，並結合構造演化特徵，預測其油氣藏類型和成藏模式。Thermolysis production of lake carbonatite organic matter and its carbon isotopic composition characteristic
湖相碳酸鹽巖有機質熱演化產物及其碳同位素組成特徵Biomarker has a wide application in the research of petroleum geology, such as different types of organics thermal evolution, ancient sediments ' environment and so on
摘要生物標志化合物在石油地質中應用廣泛，可應用於源巖有機質類型和古沉積環境評價以及熱演化階段的確定等。It is pointed out that in the studied area there exist katogene metamorphism ( area ) ; igneous contact metamorphism, where the katogene metamorphism is dominated, the igneous contacting metamorphism is only distributed in yongzheng area etc, for which the influence of thermal evolution is greatly limited
指出研究區存在深成（區域）變質和火成接觸變質兩種類型，且以深成（區域）變質類型為主，火成接觸變質類型僅分佈在永城等局部地區，對有機質熱演化的影響范圍極為有限。It has the essential source conditions for the formation of immature oil with higher abundance and better types of organic matter deposited in thicker stratum under the environment in favor of preservation of organic matter and its inversion to hydrocarbons at the early stage, as well as the appropriate maturity for abundant production of immature oil
該套泥巖不但具備有機質豐度高、類型好、單層厚度大等生成低熟油必備的物質條件以及有利於有機質保存和向烴類早期轉化的沉積環境條件，而且其熱演化程度正處于生成低熟油的高峰階段。Thermal evolution in tiandong depression, baise basin
百色盆地田東坳陷熱演化研究In this paper ， the process of hydrocarbon generation and evolution in the four thermal evolutionary stages （ low - mature ， mature ， high - mature ， overmature ） of geohistory is simulated by selecting low - mature hydrocarbon source rocks and using the method in which hydrocarbons are generated from artificial pyrolysis and petroleum migration is controlled properly
本文選用低成熟烴源巖，採取人工熱解生成油氣及適當控制石油運移的方法，模擬了4個地史熱演化階段（低熟、成熟、高熟、過熟）中油氣的生成演化過程。Because of the above mentioned reasons, the first one should be considered the main source rock in yili basin. by means of the modeling of the buried history and the history of thermal evolution, it can be concluded that this set of source rock had entered the ceiling of the oil - generating window in the early triassic period and reached its peek in the middle and end of triassic period, befor entering the highest maturity in the early and middle jurassic period, and had generating gas in the end of jurassic period
其中鐵木里克組烴源巖厚度大、有機質豐度高、成熟度高，具有較高的生烴潛力，是伊犁盆地主要的烴源巖系，通過埋藏史及熱演化史模擬，該套烴源巖於三疊紀早期已進入生烴門限，中晚三疊世達到生、排烴高峰，早中侏羅世進入高成熟階段，侏羅紀末進入生氣階段。According to the chemical experimental data of residual organic carbon content, kerogen carbon isotope, aliphaltic gas chromatography mass spectrometry of 67 outcrop specimens in the baise basin, the authors analyse the geochemical characteristics of the type and the maturation of organic matter in the lower triassic - devonian source rock
根據百色盆地周緣大量露頭樣品的殘余有機碳含量、乾酪根碳同位素、飽和烴色譜及色質等地球化學實驗數據，分析了下三疊統泥盆系海相烴源巖的有機質豐度、類型、熱演化程度。Discussion on thermal evolution and secondary hydrocarbon generation of organic matter from upper paleozoic coal measures in huabei area
華北地區上古生代煤系有機質熱演化與二次生烴探討Adiabatic geometric phase of a general quantum state
絕熱演化中一般量子態的幾何相位A quantitative model of heat production by faulting and its effect on thermal evolution of hydrocarbon source rocks
斷層作用熱模型及其對烴源巖熱演化的影響Future study should put emphasis on further improvement of tectono - thermal models and its matching with reverse models
構造熱演化正演模型的進一步完善及正、反演模型的匹配將是未來構造熱演化模擬的發展趨勢。A parameter sensitive to thermal evolution, e. g. vitrinite reflectance, is measured on a certain number of samples from a well.
對熱演化敏感的參數，例如，鏡質體反射率，可從一口井的一定數量巖樣進行測定。Application of easy ro model to the research of thermal evolution in binbei
法在濱北地區熱演化史中的應用The zhongmou depression evolutionary feature in hydrothermal stage and resource assessment
中牟凹陷熱演化特徵及其資源評價Variations of coal maceral chemistry with elevated maturity and their hydrocarbon generation
煤巖組分化學結構隨熱演化變化與生烴性研究Lagging and reaction kinetic mechanism of hydrocarbon regeneration from organic matters in coals
華北地區上古生界煤系有機質熱演化與二次生烴探討As for the second and the third source rock, they both have little potential, because they both have low maturity
小泉溝群和八道灣組由於熱演化程度低，勘探潛力小。Kinematic models have predominance in predicting heat flow but weakness in simulating basin geometry ; kinematic - rheological models are adept in tectonic modeling, but identical with kinematic models in heat flow prediction ; dynamic models contain latent advantages and also some obstacles in tectono - thermal modeling
運動學模型在預測盆地熱流演化方面具有優勢，但在預測構造沉降等幾何形態方面存在一定的缺陷；運動學流變學模型的優勢在於構造演化模擬，在熱演化方面類似於運動學模型；動力學模型蘊含著潛在的巨大優勢，只是目前還存在一些阻礙因素。分享友人