microstructures and ages of activity of the reverse faults along the southern margin of the junggar basin 準(zhǔn)噶爾盆地南緣斷裂帶顯微構(gòu)造特征與活動(dòng)時(shí)代
structural features and evolution of contemporaneous reversed faults in gas faulted depression in western qaidam basin 柴西地區(qū)尕斯斷陷同生逆斷裂構(gòu)造特征與形成演化
the most critical factors in evaluating and predicting such traps sealed by the reverse fault are the analysis of strike closure and the estimation of fault sealing 評價(jià)和預(yù)測此類圈閉的最關(guān)鍵因素是進(jìn)行走向閉合分析和斷層封閉性的評價(jià)。
based on the contrast of the comparability, the paper concludes that the footwalls of reverse faults in the front of altun mountain may form effective hydrocarbon traps 通過對比分析兩者之間的相似性,認(rèn)為柴達(dá)木盆地阿爾金山前帶構(gòu)造深部發(fā)育的逆沖斷裂下盤也應(yīng)該具有形成油氣圈閉的條件。
the research show that the formation of the fault is earlier than these klippen, but it is also a revived reverse fault after the klippen took themselves places from relationship between the fault and klippen, and the esr age determination 據(jù)斷裂帶與飛來峰壓覆及切割關(guān)系和esr年齡,表明斷裂的形成應(yīng)早于飛來峰的就位,而飛來峰就位后斷裂又有過再次的逆沖活動(dòng)。