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死海转换系大陆部分三个菱形地堑的煤级测值和热流资料,揭示出明显不同的地热状态。胡拉盆地的煤化程度剖面表明在整个晚新生代地层中地温梯度较高,平均为40℃/km。与之相似,其南35千米的加利利海亦报道有较高的热流,约1.77HFU。而更向南200千米的死海地堑的煤化程度剖面,热流数据及井底温度测值则表明,中中新世以来一直以低得多的地热状态(约0.7HFU,20℃/km)据优势。可是,地热状态的差异并不代表盆地形成机理有所不同。根据水文地质与地球物理数据的证据可以认为,北部两个盆地的高地热状态反映与附近广布的戈兰—德鲁兹火山地体有关的区域现象。因此,这种高热态与菱形地堑形成机制无关,不能用来支持非有高地热态不可的运动学模式,
The Dead Sea conversion system is based on coal-level measurements and heat flow data from three rhombic graben sections of the mainland, revealing significantly different geothermal conditions. The coal rank in the Hula basin shows a high geothermal gradient throughout the Late Cenozoic stratigraphy, averaging 40 ° C / km. Similarly, the 35-meter South Sea of Galilee reported a higher heat flow of about 1.77HFU. On the other hand, the section of coalification degree, the heat flow data and the bottom hole temperature measured at the 200-km south-east of the Dead Sea grabens show that the Central Plains has been under much lower geothermal conditions (about 0.7HFU and 20 ℃ / km) According to the advantage. However, the difference in geothermal conditions does not mean that the basin formation mechanism is different. Based on the evidence of hydrogeological and geophysical data, it can be assumed that the high geothermal state in the two northern basins reflects the regional phenomenon associated with the widespread Golan-Druze volcano. Therefore, this high thermal state has nothing to do with the formation mechanism of diamond-shaped graben, and can not be used to support kinematic modes that are not highly geothermal,