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重合後震波逆推分析台灣西南外海礦區之油氣可能分布

Post-stack Seismic Inversion Analyses for Probable Hydrocarbon Distribution in the Concession Offshore Southwestern Taiwan

摘要


上部漸新統砂岩與白堊系裂隙砂岩為台灣西南外海礦區之主要產氣層,本研究利用此區域之三維震測資料與17口井的井測資料進行重合後震波逆推分析,由聲波阻抗探討漸新統砂岩之油氣可能分布。在井測資料的使用上,由於17口井中的12口井井測資料施測區間涵蓋範圍大,合成震波比對結果較佳,故以這12口井的聲波阻抗測錄建立低頻趨勢模型,並參與重合後震波逆推計算三維聲波阻抗體。以三維震測資料與井測資料所得到的聲波阻抗結果可知,漸新統砂層頂部的聲波阻抗分布清楚看到兩個明顯的低聲波阻抗區,一個位在研究區域的南方,包含C-1、C-9、C-10、C-11與C-15等井,與C區塊相關,另外一個位在研究區域的北方,包含S-1、S-6與S-7等井,與S區塊相關。在上述C和S區塊顯示低P波阻抗的8口井,除了C-11為氣徵井外,其餘皆為氣井。此外,在本研究17口井中的8口氣井,只有C-16井在聲波阻抗平面圖上未能顯示低聲波阻抗,其餘7口井皆在漸新統砂層頂部有低聲波阻抗,顯示低聲波阻抗與油氣分布關係密切,可藉由漸新統砂層的低聲波阻抗分布來瞭解油氣的可能分布。再者,三維聲波阻抗資料可提供地質建模所需的屬性資料,做為後續地質建模之使用,以利油藏評估與油層模擬,並可做為未來此區域油氣田聯合開發決策之參考。

並列摘要


Sandstone in the Upper Oligocene series and fractured sandstone in the Cretaceous system are the main production zones in the concession offshore southwestern Taiwan. To find the probable hydrocarbon distribution, our study analyzed sand layers in the Oligocene series from three-dimensional P-impedance using post-stack seismic inversion. The result showed two low P-impedance areas at the top of the sand layer in the Oligocene series. One is located in the south of the study area which is related to the C block. The other is located in the north of the study area which is related to the S block. Low P-impedance of the sand layer correlated with hydrocarbon distribution from well log analyses. Thus we can identify the hydrocarbon distribution based on the low P-impedance distribution of the sand layer in the Oligocene series. Besides, the three-dimensional P-impedance volume provided a property model for geological modeling which facilitated resource evaluation and reservoir simulation for the decision of gas field development and production in the future.

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