中国海相油气田勘探实例之十二:塔里木盆地轮南奥陶系油气田的勘探与发现

作    者:周新源,杨海军,韩剑发,王福焕,韩杰
单    位:中国石油塔里木油田分公司
基金项目:
摘    要:
轮南奥陶系海相碳酸盐岩油气田位于塔北隆起轮南低凸起中部,是中国第一个海相碳酸盐岩特大型油气田。油气田发现于1988年,至2008年底控制垣探明油气地质储量为18.78×108 t。塔里木盆地长期构造沉积演化形成了轮南奥陶系碳酸盐岩大型古潜山及内幕背斜,潜山背斜具有古隆起控油,岩溶斜坡油气富集及准层状油气藏等特征。油气田区域性盖层为中—上奥陶统、下石炭统、上三叠统泥岩,主力烃源岩为寒武系—下奥陶统与中—上奥陶统碳酸盐岩及泥灰岩,主要目的层为奥陶系石灰岩顶面之下200m范围内的潜山岩溶缝洞型储集体与内幕层间岩溶缝洞型储集体。通过缝洞系统预测评价、酸压储层改造、稠油掺稀开采等技术攻关,勘探开发一体化管理,创新了复杂碳酸盐岩勘探开发理论与配套技术,实现了轮南奥陶系油气产量储量的快速增长。论述油气田勘探与发现的历程,剖析了取得勘探突破的实践与认识。
关键词:塔里木盆地;轮南油气田;奥陶系;海相地层;碳酸盐岩储集层;油气藏特征;油气勘探技术;勘探启示

Cases of Discovery and Exploration of Marine Fields in China (Part 12):Lunnan Ordovician Oil-Gas Field in Tarim Basin

Author's Name: Zhou Xinyuan, Yang Haijun, Han Jianfa, Wang Fuhuan, Han Jie
Institution: PetroChina Tarim Oilfield Company
Abstract:
The Lunnan Ordovician Oil-gas Field that is located in the middle part of Lunnan paleouplift that is the southern wing of Tabei Uplift is the first giant marine carbonate one in China. The field is discovered with the first achievement of high-yield industrial currents of oil and gas from Well LN-1 in May 23, 1988 and it has held the total proved oil geologic reserves in-place of 1.878×109t till the end of 2008. The top of Ordovician limestone in Lunnan area is a large and long-term weathering buried hill. An integrated anticline is developed in the inner of the buried hill. The cap beds are made up of Late Ordovician-Carboniferous-Triassic mudstone or Silurian argilla ceous sandstone and two series of source rocks are composed of Cambrian-Lower Ordovician and Middle-Upper Ordovician carbonate rocks and marlite. The main exploration targets are the carbonate karst fractured/caved reservoirs and the inside fractured/caved ones under the surface of Ordovician buried hill. The history and experi ence of exploration and exploitation with the technology and methods are reviewed in detail.
Keywords: Ordovician; Marine formation; Carbonate reservoir; Reservoir characteristics; Exploration technology;Exploration history; Lunnan Oil-Gas Field; Tarim Basin
投稿时间: 2009-02-06  
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