UC知道求石油方面英语达人帮忙翻译 百分答谢2
来源：百度知道 编辑：UC知道 时间：2024/04/27 19:00:43
FAUMAI是始新世时期沉积的，是一套海相发育的碳酸岩地层，钻井揭示地层岩性表现为褐色、灰色灰岩与白云岩互层。
依据2D seismic data解释的 FAUMAI formation,全区均有分布。从formation apparent thickness map(Fig.6-6-5)上可以看出， Formation Apparent Thickness 0-700m。总体上,构造高部位地层变薄, 局部地层有剥蚀, such as KALITAMI area;东部区域地层较厚,反映这一时期东部水体较深,沉积厚度大的特点.
SIRGA是渐新世发育的地层，是一套灰白色的灰岩，依据钻井资料西部构造高部位地层剥蚀,东部均有分布,但幅度较高的构造地层较薄.与上覆地层KAIS呈不整合接触关系。
依据2D seismic data解释的 SIRGA formation apparent thickness map(Fig.6-6-6)上可以看出， Formation Apparent Thickness 0-300m。西部构造带高点基本剥蚀,构造翼部残留地层厚度0-200m.
钻井揭示，KAIS 地层是中新世时期海相沉积的一套碳酸岩，与下伏地层成不整合接触关系，是区域标志层。
依据2D seismic data解释的 KAIS formation apparent thickness map(Fig.6-6-7)上可以看出，Formation Apparent Thickness 150-350m。构造高部位地层较薄，西部构造带表现较突出。KAIS formation 是一套有利的储层，在邻区均有油气发现。
钻井揭示，STEENKOOL 地层发育较厚，大体可划分3个岩性段。依据地震特征，Lower STEENKOOL 地震响应明显，容易识别。
依据2D seismic data解释的 Lower STEENKOOL formation apparent thickness map(Fig.6-6-8)上可以看出，Formation Apparent Thickness 150-400m，工区内发育稳定。该套地层泥岩和灰岩发育
FAUMAI is deposited during the Eocene, is a marine carbonate rock strata development, the performance of drilling for lithology revealed brown, gray limestone and dolomite interbedded.
Based on 2D seismic data interpretation FAUMAI formation, both the distribution of the whole region. From the formation apparent thickness map (Fig.6-6-5) can be seen, Formation Apparent Thickness 0-700m. Overall, the structural parts of stratigraphic thinning high, there is erosion of local stratigraphy, such as KALITAMI area; the eastern part of the regional stratigraphic thick, the eastern part of this period reflect the deeper water, sediment thickness large.
Is SIRGA Oligocene strata development, the limestone is a gray, based on drilling data the western part of formation of high tectonic denudation, the distribution of the eastern part of both, but a higher rate of formation of the thin structure. KAIS and overlying strata was not integrated contact relationship.