The relation between heat flow obtained by curie depth point (CDP) and the faults and gas leaks in the black sea

Tutunsatar He, Dolmaz Mn, O. E., Okyar M, Kalyoncuoglu Uy, Starostenko Vi, Kutas Ri, Rusakov Om, Legostaeva Ov, Hisarli Zm
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Abstract

CDP values were measured. They range from 22km to 38km. The deepest CDP values are observed in the Black Sea basins where the sediment thickness is high, while the shallowest values are observed in the middle Black Sea ridge, and in the thin sedimentary regions of the coast. The Central Black Sea ridge generally ranges from 22 to 28 km. From the CDP values, the heat gradient and corresponding heat flow values were also obtained. Heat flow values of the Black Sea basin range from 22 to 41mW/m2. When the relationship between the deep faults and gas leaks with the heat flow is examined, it is observed that the possible deep fault zones and gas migration places correspond to a higher heat flow value than the average heat flow.
由居里深度点(CDP)获得的热流与黑海断层和天然气泄漏的关系
测量CDP值。射程从22公里到38公里。在沉积厚度较高的黑海盆地,CDP值最深,而在黑海中部海脊和海岸薄沉积区,CDP值最浅。黑海中部海脊的长度一般在22至28公里之间。从CDP值可以得到热梯度和相应的热流值。黑海盆地热流值在22 ~ 41mW/m2之间。当考察深断层与气体泄漏与热流的关系时,发现可能的深断层带和气体运移位置对应的热流值高于平均热流值。
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