REVEALING DEEP CONDENSATE GAS RESERVOIR IN A ARCHEOZOIC METAMORPHIC BURIED HILL RESERVOIR BY ULTRASONIC IMAGE LOGS, SPECTROSCOPY LOGS AND CORE DATA, BOHAI BAY BASIN, EASTERN CHINA

Bo Liu, Guoqiang Zhang, Xianlei Zeng, Jiheng Zhou
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Abstract

The Archeozoic metamorphic buried hill reservoir of Bozhong Sag in Bohai Bay Basin is a proven condensate gas reserves over 100 billion cubic meters. Clear understanding on buried hill vertical zones variation is vital to characterize reservoir quality and reservoir distribution. Conventional core samples analysis is far than enough to characterize the complexity and diversity of basement reservoir. Weathering, lithofacies, and fracture network also play important role in controlling the reservoir property. The fractures in the target area are unevenly developed due to the multi tectonic activities and stress field rotation during the initial period of the basement evolution. In addition, the mineral’s composition of the basement lithofacies is complex due to the metamorphism, alteration and weathering which further affect the reservoir quality. Characterizing effective fracture distribution of the basement lithofacies across the area is crucial to classify the good reservoir zonation. However, identifying fracture by electrical resistivity borehole image endured high uncertainty as conductive fracture are possibly filled by clay, iron minerals (pyrite or siderite) or mud filtrate. Ultrasonic image logs can identify different fracture based on both the amplitude image and transit time image, which can clearly identify effective or non-effective fractures. In total, four types of fractures are identified: closed fractures, fully open fractures, partially open fractures, and vuggy open fractures. Based on the lithofacies, fracture development, volumetric minerals from spectroscopy logs and conventional logs, the archeozoic metamorphic buried hill was revealed zone by zone. Strongly weathered zone, sub weathered zone and insider buried hill zone were proposed. The reservoir quality, lithofacies identification, multi well fracture development analysis by three buried hill zones and production controlling factors were fully demonstrated in this study.
利用超声波图像测井、光谱测井和岩心数据揭示中国东部渤海湾盆地原生变质埋藏山储层中的深层凝析气藏
渤海湾盆地渤中沙砾地的新生代变质埋藏山体储层已探明凝析气储量超过 1000 亿立方米。清楚地了解埋藏丘陵垂直带的变化对于确定储层质量和储层分布至关重要。常规的岩心样品分析远不足以描述基底储层的复杂性和多样性。风化、岩性和断裂网络在控制储层性质方面也起着重要作用。由于基底演化初期的多构造活动和应力场旋转,目标区域的断裂发育不均。此外,由于变质、蚀变和风化作用,基底岩性的矿物成分复杂,进一步影响了储层的质量。确定整个地区基底岩性的有效断裂分布特征对于划分良好的储层分带至关重要。然而,通过电阻率井眼图像识别断裂具有很高的不确定性,因为导电断裂可能被粘土、铁矿物(黄铁矿或菱铁矿)或泥浆滤液填充。超声波图像测井可根据振幅图像和传输时间图像识别不同的裂缝,从而明确识别有效或无效裂缝。总共可识别出四种类型的断裂:闭合断裂、完全开放断裂、部分开放断裂和伏流开放断裂。根据岩性、断裂发育、光谱测井和常规测井的体积矿物,逐区揭示了原生代变质埋藏山体。提出了强风化带、亚风化带和内埋山带。该研究充分论证了三个埋藏山带的储层质量、岩性识别、多井裂缝发育分析以及生产控制因素。
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