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James Lime: A General Introduction

机译:詹姆斯·莱姆:概述

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The James Limestone is a Lower Cretaceous (Upper Aptian) carbonate interval distributed regionally across the northern rim of the Gulf of Mexico Basin, from eastern Texas to offshore Florida. Significant oil and gas production from the James has existed since the 1960 discovery of Fairway Field in the East Texas Basin. This very large oil accumulation (~400 million bbls oil-in-place), characterized by very high rates of recovery (EUR > 230 million bbls), established the James as a target of exploratory interest. While no other field of similar size has been found in the formation during the succeeding four decades, recent drilling in both onshore and offshore areas of the northern Gulf has established important new gas resources in the James.
机译:詹姆士石灰岩是下白垩统(上Aptian)碳酸盐岩层段,分布在墨西哥湾盆地北缘,从德克萨斯州东部到佛​​罗里达州近海。自从1960年在东德克萨斯盆地发现Fairway油田以来,詹姆斯就已经大量开采了石油和天然气。大量的石油积累(约4亿桶原位石油)具有很高的采收率(> 2.3亿欧元/桶),使詹姆斯成为勘探兴趣的目标。尽管在随后的40年中没有在该地层中找到其他类似规模的气田,但最近在北部海湾北部陆上和海上地区进行的钻探已在詹姆斯地区建立了重要的新天然气资源。

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