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Characteristics and Formation Conditions of Oil/Gas Fields (Pools) in Abnormal Formation Pressure Environments in China

机译:中国异常形成压力环境中油/气田(池)的特性和形成条件

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Abnormal pressure oil/gas fields (pools) are widely distributed in China, which with the less than 0. 9 and greater than 1. 1 pore fluid pressure coefficient account for 42% of total oil/gas fields (pools) ,35% of which are overpressured ones and 7%, subpressured ones. The abnormally low pressured gas fields (pools) are relatively less in numbers and each has less than 5X 10'm3 in reserves) the number of super-pressured gas fields (pools) is more than that of the former, but decrease with the increasing of pore fluid pressure coefficient, and reserves range from 2X10'm3 to 15X 109m3. The spatial and temporal distribution, the abnormally pressured oil/gas fields (pools) are chiefly located at the formations with composite lithological-structural traps and lithological traps from the Paleozoic to the Cenozoic. Their stages of accumulation were generally in the Mesozoic and the Tertiary. The aubpres-sured oil/gas (pools) were buried at a depth of less than 2000m, and the overpressured ones at a depth of more than 3500m. The more the depth is, the more the number of overpressured oil/gas fields (pools) becomes obviously. The sedimentary-type overpressured oil/gas fields (pools) are mainly located in the eastern area of China , and controlled by the under-compaction, aquathermal, hydrocarbon generation and dehydration of clay minerals which all are the contributors to the pore fluid pressures. But in the central area of China, the structural-type overpressured oil/gas fields (pools) were mainly influenced by the hydrocarbon generation and the tectonic compression in the late stages. The subpressured oil/gas fields (pools) in northeast area of China are chiefly controlled by the tectonic elevation and erosion in the late stages. Our investigation shows that the very favorable conditions to form abnormally high pressure oil/gas fields (pools) in China include the abundant soure rocks, the matching of hydrocarbon generation with the tim-ing of traps, the effective regional seals and the pore fluid pressure coefficient between 1.1-1.3.
机译:异常的压力油/天然气场(游泳池)在中国广泛分布,其中少于0. 9且大于1.1孔隙流体压力系数占油/天然气场(池)的42%,35%这是过度抑制的,7%,后抑制。异常低压的气体场(池)的数量相对较低,每个储量少于5倍10'm3)超压气田(池)的数量比前者的数量大,但随着增加的增加而降低孔隙流体压力系数,储量范围为2×10'm3至15x109m3。空间和时间分布,异常加压的油/气田(池)主要位于具有复合型岩性结构陷阱的地层和来自古生代到新生代的岩性疏水阀。它们的积累阶段通常在中生代和三级中。将Aubpres-Sured油/气体(池)埋入小于2000米的深度,并且过度超过3500米的过度压抑。深度越多,过压油/气田(池)的数量就越多于明显。沉积型过压石油/天然气场(游泳池)主要位于中国东部地区,并由粘土矿物质的含量,水疗,碳氢化合物产生和脱水的控制,所有这些都是孔隙流体压力的贡献者。但在中国的中心地区,结构型过度型油/天然气(池)主要受到碳氢化合物产生和后期构造压缩的影响。中国东北地区的被抑制油/天然气场(游泳池)主要受到后期构造海拔和侵蚀的影响。我们的调查表明,在中国形成异常高压油/天然气(游泳池)的有利条件包括丰富的源岩,碳氢化合物产生与陷阱的匹配,有效的区域密封和孔隙流体压力1.1-1.3之间的系数。

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