Depositional Facies, Diagenetic Terranes, and Porosity Development in Lower Ordovician Ellenburger Dolomite, Puckett Field, West Texas
Depositional Facies, Diagenetic Terranes, and Porosity Development in Lower Ordovician Ellenburger Dolomite, Puckett Field, West Texas
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DOI：
10.1007/978-1-4612-5040-1_2
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发表时间：
1985-12
影响因子：
--
通讯作者：
R. Loucks;James H. Anderson
中科院分区：
文献类型：
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作者：
R. Loucks;James H. Anderson
帕克特油田位于德克萨斯州西部的佩科斯县，位于埃尔帕索东南偏东约220英里（360公里），米德兰西南90英里（145公里）（图1-1）。发现井，菲利普斯石油公司1号格伦纳，于1952年完成，总深度为16,575英尺（5052米），最初每天生产1200万立方英尺天然气（340 000立方米）和38桶石油，来自埃伦堡白云岩的穿孔（下奥陶统）在13，700至14，285英尺（4165-4343米）（布兰查德，1977年）。截至1979年1月，该油田有35口生产威尔斯井。
The Puckett Field is located in Pecos County, west Texas, approximately 220 miles (360 km) east-southeast of El Paso and 90 miles (145 km) southwest of Midland (Fig. 1-1). The discovery well, the Phillips Petroleum Co. No. 1 Glenna, was completed in 1952 at a total depth of 16,575 feet (5052 m), with an initial production of 12 million cubic feet of gas per day (340,000 m3) and 38 barrels of oil per day, from perforations in the Ellenburger Dolomite (Lower Ordovician) at 13,700 to 14,285 feet (4165–4343 m) (Blanchard, 1977). As of January 1979, the field had 35 producing wells.