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1热液场的构造梅内兹·格文热液场位于大西洋中脊海洋裂谷段拉基·斯特拉依克场以北(37°35′~38°N之间)。在该区,亚速尔热点对岩石圈板块张开区的地形产生了实质性的影响。当接近热点时,内部裂谷的深度减小,裂谷谷地实际上消失了。在梅内兹·格文场发育区内,主要的构造是底部
STRUCTURE OF THE HYDROTHERMAL FIELD The Menez-Gwin hydrothermal field is located north (37 ° 35 ’~ 38 ° N) north of the Raki Stellaker field in the mid-oceanic ridges. In this area, the Azores hot spots have had a substantial impact on the topography of the lithospheric plate open area. As the hot spot approaches, the depth of the internal rift decreases and the rift valley virtually disappears. In the Menez Gwen field development zone, the main structure is the bottom