Science. 1978 Oct 27;202(4366):427-9. doi: 10.1126/science.202.4366.427.
Remarkable folding and uplifting movements were active along the western margin of the Sinai subplate (the Bardawil Lagoon and its periphery) during the Upper Holocene. The coasts of the eastern margin (Gulf of Elat) were also uplifted during the same tectonic phase. The nature of this activity is discussed in relation to the regional tectonic framework.
在上全新世期间，西奈亚板块西部边缘（巴达维湖及其周边地区）发生了显著的褶皱和隆升运动。同一构造阶段，东部边缘（埃拉特湾）的海岸也发生了抬升。本文讨论了这种活动与区域构造框架的关系。
