thick source 中文意思是什麼
thick source
解釋
厚源-
Based on available data, the study on regional structure, sedimentary reservoir and source rock characteristics shows that the basins in south china sea had experienced sedimentary evolution in faulting period and depression period, deposited thick cenozoic formation, upwardly developed alluvial fan facies, river - lake facies coastal swamp facies coastal facies, neritic facies and bathyal deposit system, regionally had 3 source rocks of eocene, oligocene and miocene, 3 reservoirs of pre - cenozoic basement buried bill, oligocene sandstone and miocene reef, with pliocene and pleistocene neritic facies and bathyal shale as regional caprock
摘要以現有資料為基礎，通過對區域構造、沉積儲層、烴源巖特徵等基礎石油地質條件研究，認為南海海域各盆地經歷了斷陷期和坳陷期沉積演化，沉積了巨厚的新生代地層，自下而上發育了沖積扇相、河湖相、濱岸沼澤相、濱海相、淺海相、半深海相沉積體系，區域上存在始新統、漸新統和中新統3套烴源巖，前新生代基巖潛山、漸新統砂巖、中新統生物礁3套儲層，區域蓋層為上新統和更新統淺海半深海相泥巖。 -
Dongpu sag is of the superior geological conditions for forming deep gas pools, including two sets f premium source rocks, variety of sand bodies, sell developed porosity and thick halite and mudstone as cap rocks
摘要東濮凹陷具有形成深層氣的優越基礎地質條件：兩套優質烴源巖、多種類型的儲集砂體和高異常孔隙發育、厚的巖鹽和泥巖作為良好蓋層。 -
The causes are discussed from aspects of oil - gas source beds, trapping and storing space, oil - gas migration channel and thick proofing layers, oil - gas maturity stage and allocation of effective trapping stage, suggesting the searching of primary oil - gas pool of the cambrian and lower ordovician at the relatively shallow layers and surrounding places with faults developed
從油氣源層、圈閉與儲集空間、油氣運移通道與巨厚隔層、油氣成熟期與圈閉有效期配置等四個方面探討了未獲油氣之原因，提示在滿加爾坳陷腹地，相對較淺部位及周邊斷裂發育部位尋找寒武系和下奧陶統的原生油氣藏。 -
Futhermore, the formation of reservoir experienced four periods : the first, from esi to ed ; the second, from late ng to early nm ; the third, nm ; the fourth, from late nm to now. so we predict that exploration in qianmiqiao should be mainly directed to condensed oil and gas reservoir nearby banqiao depression and gas reservoir is more probably found near qikou depression. 8. analogue of the conditions required for reservoir formation in huanghua buried hills shows that, high quality and thick es3 hydrocarbon source rock distributed richly in the middle area depression, and moderate quality sandstone distributed in south area, but the match bet
8對黃驊坳陷區「新生古儲」型潛山成藏條件的類比分析表明，中區凹陷中分佈有厚度較大的優質沙三段烴源巖，南區分佈有較好的孔二段烴源巖，但中區千米橋地區生儲配置比南區好，因此，整體上中區千米橋潛山一帶油氣藏的勘探前景優于南區。 -
The features of these sequences arerbefore sequence i deposited during the rapid subsidence of the depression, the range of the sediment is limited. sequence ii is the first series of source and reservoir rocks of the depression. there are regional unconformity at the bottom of the sequence iii. the rock type are variety. this sequence is evaluated as good source rock, sequence iv is associated with the first section of duhongmu formation, thick mudstone at the bottom and the thick single sandston are the main rock type. this sequence are evaluated as good source rock and reservoir. sequence v associated with the second and the third section of duhongmu. which is mainly mudstone and can be regional capping rocks
層序對應于阿爾善組二段，為深色泥巖與砂礫巖不等厚互層，是本區的第一套烴源巖和儲集層，可以作為本區儲層。層序對應騰格爾組，此時凹陷擴張，沉積層底部具有區域性的沖刷面，巖性變化大，是較好的生油層。層序對應都紅木組一段，下部泥巖發育，單砂層較厚，是主要的生油層和儲層。 -
Based on the research into sedimentary microfacies, source rocks and associations of source rock, reservoir rock and caprock, the paper discusses the formation mechanism of thick oil in detail and summarizes the transportation and accumulation regular of oil - gas in study area
該文在對沾化凹陷羅家鼻狀構造沙四上段沉積微相、生油巖條件和生儲蓋組合綜合研究基礎上，詳細論述了稠油的形成機制，總結了該區油氣運移和富集規律。 -
The biomarker characteristics of these two types of viscous oils are distinctive. oil source correlation results show the altered viscous oils were generated from the es3 source rocks and subsequently suffered biodegradation, oxidation and water washing effects near the surface. there exists huge thick alluvial glutinite in luojia - kenxi area, with various physical properties
兩類稠油生物標志物組成也有明顯的差異，次生稠油主要由來源於沙三段源巖的正常原油（稀油）經生物降解、地表氧化、水洗等次生作用形成的，並且成熟度指標相對較高。 -
On the basis of analysis on the characteristics of structural evolution, the growth of the source rocks is analyzed. in the period of mesozoic - palaeozoic, caledonian events and the evolution of hercynian - early indo - chinese cycle are experienced in two - phase marine passive continental margin and craton basin in the lower and middle yangtze region, by which stable enormous thick mesozoic - palaeozoic deposites are induced, six sets of source rocks are produced, it has a strong capacity of hydrocarbon generation
摘要通過構造演化特徵分析了海相烴源巖的發育，中、下揚子區中古生代經歷了加里東和海西早印支旋迴兩個階段的海相被動大陸邊緣和克拉通盆地演化，形成了巖性穩定的巨厚中古生界，發育了6套烴源巖，具有較強的生烴能力。 -
In non - destructive x - ray fluorescence analysis with thick target, correction method for difference in fluorescence intensity of elements due to sample shape and different distance to the source detector with yttrium as an outer mark element was studied
摘要在厚靶的非破壞性x射線螢光分析中，以釔做外標元素，研究了不同樣品形狀及與源、探測器距離不同時，引起接收到元素螢光強度差異的校正方法。 -
Water quality - radiological methods - measurement of gross alpha activity in non - saline water : thick source method
水質.第3部分:放射性法.第1節:不含鹽的水中總活度測量:厚源法 -
Carboniferous strata, more than 1000m in thick in the area of hexi corridor to bayan haot basin, is the coal measures of transitional phase, in which there are three kinds of hydrocarbon source rocks including dark mudstone, limestone, coal and carbonaceous mudstone
摘要河西走廊至巴彥浩特盆地地區石炭紀地層厚逾千米，是一套海陸交互相含煤巖系，發育暗色泥巖、灰巖、煤層及碳質泥巖等3大類烴源巖。
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