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PROCESS FOR PREDICTING THE QUANTITY AND COMPOSITION OF FLUIDS PRODUCED BY MINERAL REACTIONS OPERATING IN A SEDIMENT BASIN

机译:预测沉积盆地中矿物反应产生的液体的数量和组成的过程

摘要

A method for predicting the amount and composition of fluids produced by mineral reactions operating in a sedimentary basin, and trapped with hydrocarbons in the reservoirs. Characteristic geological data of the basin are acquired and a representation of the basin is constructed by a mesh. Then, for at least one set of meshes of the mesh, and using a basin model and geological data, the following parameters are calculated: a depth of burial (z), a temperature (T) , a pore pressure (P), a volume (V) and a porosity (Φ) at successive ages (ti) representative of the geological history of the basin. In each mesh of the set of meshes, a mineralogical or chemical composition of rock is determined from the geological data of the basin. Finally, the quantity and the composition of fluids of mineral origin are determined within the set of meshes, by means of a geochemical model and an equation of state, from said parameters, of said composition, and a thermodynamic database.
机译:一种预测在沉积盆地中进行的矿物反应产生的并被碳氢化合物捕集的流体数量和组成的方法。获取盆地的特征地质数据,并通过网格构建盆地的表示。然后,对于至少一组网格,并使用盆地模型和地质数据,计算以下参数:埋藏深度(z),温度(T),孔隙压力(P),代表盆地地质历史的连续年龄(ti)的体积(V)和孔隙率(Φ)。在该组网格中的每个网格中,根据盆地的地质数据确定岩石的矿物学或化学组成。最后,借助于地球化学模型和状态方程,从所述参数,所述组成和热力学数据库中,在一组网格内确定矿物来源的流体的数量和组成。

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