摘要
火14井北断块构造位于准噶尔盆地东部隆起沙帐断褶带北端,目的层为二叠系平地泉组,主体处于石炭系火山岩逆掩推覆体之下,由于受上覆不等厚火山岩高速层的影响,该断块内二叠系层速度横向变化快、干扰波发育、地震资料品质差。复杂的速度变化制约了对断块内构造形态的认识及该区油气勘探的突破。对此,分别采用地质模型正反演技术分辨出了火山岩体其展布和接触关系,在此基础上,分析其波形及属性特征,落实了火山岩推覆体掩伏构造形态和构造高点,同时用变速成图技术提高了构造成图精度。
Well Huol4 north fauh block is located in north side of Shazhang bruchfalten zone in Eastern uplift of Junggar basin. The tar- get interval is tile Permian Pingdiquan formation, the nmin part is generally heneath the carboniferous voh＇anic overthrust nappe. Afteeted by the overlying unequal thickness volcanic high-speed zone, the Permian in this block is of charaeteristies of fast change of lateral interval velocity, developing interference wave and poor quality of seismic data. So the complex velocity changes restrict understanding of structural features within the block and technological breakthrough in oil-gas exploration in this area. In this paper, the volcanic rock body, its distri- bution and contact relationship are distinguished using the fnrward anti inversion techniques of geological model, based on which by analyz- ing the waveform and attribute characteristics, the volcanic overthrust nappe structural shape and highs are defined. Meanwhile, using velocity-varied mapping technique improves the structural mapping accuracy.
出处
《新疆石油地质》
CAS
CSCD
北大核心
2012年第5期564-565,共2页
Xinjiang Petroleum Geology
基金
中石油新疆油田分公司重点科研攻关项目(2010215)
关键词
准噶尔盆地
地质模型
反演
正演
火山岩
Junggar basin： the geological model： inversion
forward
volcanic rock
