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首页> 外文期刊>Earth Sciences >Present-Day Two-Dimension Maturity History Modelling of Source Rocks from the Central Region of the Andaman Sea Back Arc Depression
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Present-Day Two-Dimension Maturity History Modelling of Source Rocks from the Central Region of the Andaman Sea Back Arc Depression

机译:来自安达曼海背弧凹陷中部地区烃源岩的当今二维成熟度历史模拟

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Basin modelling is an essential research tool that aids geologists improve the description and analysis of subsurface activity. The central region of the Andaman Sea back arc basin is a potential oil and gas prospect. Herein, two-dimension present-day maturity models are constructed from four seismic sections of the study area using Basin Mod software (Platte River Associates, Inc. of USA). Designated study areas are the South to North Moattama Basin, western Moattama to the Mergui Shelf, Western to Eastern Moattama basin centres through Eastern Moattama basin centre to the Eastern section of Mergui basin and Eastern Andaman Sea Basin to Western Mergui Basin. The two-dimension (2D) maturity models are generated from known data burial and geothermal data. Vitrinite Reflectance (Ro%) which is the main variable in determining source rock (s) maturity showed that the source units were within the oil (0.5% ≤ Ro ≤ 1%) and gas (1.3% ≤ Ro ≤ 4.5%) and had commenced generation of some quantities of hydrocarbons. Data analyzed revealed that most portions of the Oligocene and Lower Miocene shales source units in all study areas buried below 2000 m are matured to generate oil and/or gas. The outcome of modelling also indicated that source units from the Moattama Basin center and the Mergui Basin were mostly matured to produce some form of hydrocarbons, principally gas or dry gas. However, no oil expulsion into limestone reservoirs was observed; only gas or dry gas.
机译:盆地建模是必不可少的研究工具,可帮助地质学家改善地下活动的描述和分析。安达曼海背弧盆地的中部地区是潜在的油气前景。在此,使用Basin Mod软件(美国Platte River Associates,Inc.)从研究区域的四个地震剖面构建了二维当今成熟度模型。指定的研究区域是南至北Moattama盆地,西至Moattama至Mergui陆架,西至东Moattama盆地中心,东至Moattama盆地中心至Mergui盆地的东部,东安达曼海盆地至西部的Mergui盆地。二维(2D)成熟度模型是根据已知的数据埋藏和地热数据生成的。玻璃体反射率(Ro%)是确定烃源岩成熟度的主要变量,显示源单元在油(0.5%≤Ro≤1%)和天然气(1.3%≤Ro≤4.5%)内并且具有开始产生一些碳氢化合物。分析的数据显示,埋在2000 m以下的所有研究区域中的渐新世和下中新世页岩气源单元的大部分已成熟,以产生石油和/或天然气。建模结果还表明,来自莫阿塔马盆地中心和梅尔圭盆地的烃源单元大多已经成熟,可以生产某种形式的碳氢化合物,主要是天然气或干气。但是,没有观察到石油排入石灰岩储层。只有气体或干燥气体。

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