首页> 外文会议>GCSSEPM Foundation Bob F Perkins Research Conference >Origin of Lower Pliocene Remobilized Deepwater Mounded Deposits, Yafo Formation, Levant Basin, Southeastern Mediterranean: A Head-Scratching, Group Exercise to Explain Mounded Deposits
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Origin of Lower Pliocene Remobilized Deepwater Mounded Deposits, Yafo Formation, Levant Basin, Southeastern Mediterranean: A Head-Scratching, Group Exercise to Explain Mounded Deposits

机译:低级全茂的起源重新染色深水土墩矿床,Yafo形成,Levant Basin,东南地中海:头部划伤,群体练习来解释土墩矿床

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摘要

The Levant basin is located in the southeastern portion of Mediterranean Sea (Fig. 1). The basin is bordered by the African plate to the south, the Sinai plate to the south and east, and the Eurasian plate to the north (Fig. 1). Although there has been significant petroleum exploration to the west in the Nile Delta region (Fig. 1), there has been substantially less success in the Levant basin between the late 1960 to late 1990's (Gardosh et al., 2008).
机译:Levant Basin位于地中海的东南部(图1)。该盆地与南部的非洲板块接壤,西奈板到南部和东部,欧亚板块到北方(图1)。虽然在尼罗三角洲地区向西有重要的石油勘探(图1),但在1960年代后期到1990年末(Gardosh等,2008),Levant盆地的勒维盆地取得了大幅取得成功。

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