首页|基于加权平均算法的丽水凹陷剥蚀量恢复及对沉积的控制

基于加权平均算法的丽水凹陷剥蚀量恢复及对沉积的控制

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丽水凹陷是东海陆架盆地油气勘探的主战场之一,由于受多期次构造运动改造,地层发生明显的隆升剥蚀致使对丽水凹陷原型盆地认识不清,尤其制约了对凹陷内烃源岩及储层分布的认识.本文从剥蚀量恢复的关键参数入手,综合趋势外延法、声波时差法、镜质体反射率法及沉积速率法等综合厘定关键不整合面剥蚀量厚度,结合残余厚度和去压实矫正恢复其原始层厚度,在沉积补偿原理控制下恢复了丽水凹陷灵峰组至温州组"早期分隔,晚期联通,中心东移"的古地貌特征.在古地貌及沉积相分析的基础上,建立了隆起-斜坡-凹陷控制下的沉积体差异展布模式,古地貌系统研究为丽水凹陷下一步烃源岩评价及有利储层展布评价提供有力的理论支撑.
Restoration of erosion amount and control of sedimentation in Lishui depression based on weighted average algorithm
The Lishui depression is one of the main battlefields for oil and gas exploration in the East China Sea shelf basin.Due to multiple tectonic movements and significant uplift and erosion of the strata,the understanding of the prototype basin of the Lishui Depression is unclear,especially restricting the understanding of the distribution of hydrocarbon source rocks and reservoirs in the depression.Starting with the key parameters of the denudation recovery,this paper determined the denudation thickness of the key unconformity by comprehensive trend epitaxy method,acoustic time difference method,vitrinite reflectance method and sedimentation rate method.The original layer thickness is restored by combining the residual thickness and decompacting correction.Under the control of sedimentary compensation principle,the paleogeomorphic features of"early separation,late connection,center shifting east"from Lingfeng Formation to Wenzhou Formation in Lishui Sag are restored.Based on the analysis of paleo-geomorphology and sedimentary facies,the differential distribution model of sedimentary bodies under the control of uplift,slope and depression is established.The study of palaeo-geomorphic system provides strong theoretical support for the further evaluation of hydrocarbon source rocks and favorable reservoir distribution in Lishui depression.

Lishui depressionrestoration of erosion volumepalaeogeomorphology

李帅、余政宏、王宇

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中海石油(中国)有限公司上海分公司,上海 200335

丽水凹陷 剥蚀量恢复 古地貌

中国海油"七年行动计划"东海专项

CNOOC-KJ135 ZDXM 39 SH02

2024

上海国土资源
上海市地质调查研究院 上海市地质学会

上海国土资源

CHSSCD
影响因子:1.435
ISSN:2095-1329
年,卷(期):2024.45(1)
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