石油实验地质
石油實驗地質
석유실험지질
EXPERIMENTAL PETROLEUM GEOLOGY
2013年
5期
473-479,486
,共8页
金之钧%刘光祥%方成名%张长江%彭金宁
金之鈞%劉光祥%方成名%張長江%彭金寧
금지균%류광상%방성명%장장강%팽금저
下组合%上组合%烃源灶%盖层%源-盖匹配%海相油气勘探%下扬子区
下組閤%上組閤%烴源竈%蓋層%源-蓋匹配%海相油氣勘探%下颺子區
하조합%상조합%경원조%개층%원-개필배%해상유기감탐%하양자구
lower assemblage%upper assemblage%hydrocarbon kitchen%cap rock%source and cap rocks control hydrocarbon%petroleum exploration in marine strata%Lower Yangtze
下扬子区中古生代发育了多类型的盆地,构建了海相下组合、上组合2套成油气组合,但受印支期-中燕山期、晚燕山期-喜马拉雅期构造改造和盆地叠加,海相层系油气生成演化、运聚成藏十分复杂,难以用传统的方法进行有利区带优选。从“源-盖控烃”出发,通过对加里东末期、印支末期、中燕山末期及现今等关键时期烃源灶与盖层的匹配组合关系研究和有利油气聚集与保存区的预测,利用多层多期多元复合成藏预测模型预测了有利油气勘探区。
下颺子區中古生代髮育瞭多類型的盆地,構建瞭海相下組閤、上組閤2套成油氣組閤,但受印支期-中燕山期、晚燕山期-喜馬拉雅期構造改造和盆地疊加,海相層繫油氣生成縯化、運聚成藏十分複雜,難以用傳統的方法進行有利區帶優選。從“源-蓋控烴”齣髮,通過對加裏東末期、印支末期、中燕山末期及現今等關鍵時期烴源竈與蓋層的匹配組閤關繫研究和有利油氣聚集與保存區的預測,利用多層多期多元複閤成藏預測模型預測瞭有利油氣勘探區。
하양자구중고생대발육료다류형적분지,구건료해상하조합、상조합2투성유기조합,단수인지기-중연산기、만연산기-희마랍아기구조개조화분지첩가,해상층계유기생성연화、운취성장십분복잡,난이용전통적방법진행유리구대우선。종“원-개공경”출발,통과대가리동말기、인지말기、중연산말기급현금등관건시기경원조여개층적필배조합관계연구화유리유기취집여보존구적예측,이용다층다기다원복합성장예측모형예측료유리유기감탐구。
From Paleozoic to Mesozoic, multiple types of basins developed in the Lower Yangtze region, forming 2 sets of petroleum assemblages of marine facies ( the lower one and the upper one) . Influenced by the tectonic deformation and basin superposition during Indosinian-middle Yanshanian and late Yanshanian-Himalayan periods, the generation, evolution, migration and accumulation of petroleum in marine strata are very complicated. As a result, it is difficult to select favorable zones for petroleum exploration in traditional ways. Based on the theory of“source and cap rocks control hydrocarbon”, the relationships between hydrocarbon kitchen and cap rock at the end of Caledonian, the end of Indosinian, the end of middle Yanshanian and present days are discussed, and the favorable zones for petroleum accumulation and preservation are predicted. An accumulation prediction model of multiple layers, stages and elements is applied to point out favorable zones for exploration.