1) M5_4~1
马五_4~1
1.
THE STUDY OF DIAGENETIC PHASES AND PREDICTION OF PROSPECTIVE RESERVOIRS IN M5_4~1 GAS-BEARING FORMATION IN THE CENTER OF ORDOS BASIN;
陕甘宁盆地中部马五_4~1气层成岩相与有利储集区预测
2) Ma5_4~1 member
马五_4~1段
4) the Ma5_4~1 member
马五_4~1地层
1.
Karstification had the important impact on The Ma5_4~1member,due to the denudation the northwestern lost strata of Shan231 block made it unconformable to the Neopaleozoic Carboniferous System,not having been eroden by the paleogutter to the Ma5_4~1 member,the northwestern zone is the key factor of dominating the karstification of Shan231 Block.
陕231井区位于靖边古潜台西北边部,北东高,南西低,马五_4~1地层受岩溶影响强,由于剥蚀作用造成陕231井区西北部马五_4~1地层缺失,使其下覆地层与上古生界石碳系地层呈不整合接触,同时由于古沟槽均未切割至马五_4~1地层,所以西北部地层缺失区是控制陕231井区岩溶作用的主要因素。
5) Ma-jiagou formation
马五_4段
6) Ma 5 1 reservoir
马五1储层
补充资料:五马渡江
1.指西晋末司马氏五王南渡长江,于建邺(今南京)建立东晋王朝事。
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