On spatial variability of ferro-manganese nodule fields (poligon Clarion-Clipperton)Ilyin, A VIlyin, A VBogorov, G VBogorov, G VSkornyakova, N SSkornyakova, N S
The deep seafloor of the Northeastern Pacific Ocean between the Clarion and Clipperton Fracture Zones (CCZ) hosts large deposits of polymetallic nodules th
国际上习惯将北东太平洋克拉利昂断裂带和克利帕顿断裂带之间的区域称为C—C区(zone Clarion-Clipperton),该区是太平洋内()的最富集矿区。A.多金属结
Raschka U,Kersken D,Scuckas H,Menot L,Bonifacio p,vanreusel a,macheriotou l,cunha m,hilárioa,rodrigues c,colaçoa,里贝罗p,błaewiczm,古老的a,jones d,比尔特d,Goineau A,Amon D,Smith C,Patel T,McQuaid K, Spickermann R,Brager S(2016)伦敦研讨会关于Clarion-Clipperton区的生物地理和...
The results of recent studies of specific craterlike structures in sediments of the Clarion-Clipperton zone (CCZ) of the Pacific Ocean are summarized. It was established from the example of a crater located in the bottom area with age of 40 Ma that such craters from several hundreds of ...
M., Picard, A., Ruhlemann, C., Eisen- hauer, A., Kuhn, T., Ziebis, W., and Kasten, S.: Diffusive trans- fer of oxygen from seamount basaltic crust into overlying sedi- ments: an example from the Clarion-Clipperton Fracture Zone, Earth Planet. Sc. Lett., 433, 215-225, 2016....
海底4000 米处的深海里实际上是一个完全没有光明的黑暗世界。 然而,研究表明,在这样一个黑暗的世界中可能会产生氧气。 它位于太平洋的 Clarion Clipperton 水域。 这是一块巴掌大小却很神秘金属质岩石。 正是这块岩石在 4,000 米深处产生氧气。 长期以来,该地区经常被勘探,以提取岩体中丰富的稀有金属,例如锰、铜...
ISA, 2010. A Geological Model of Polymetallic Nodule Deposits in the Clarion-Clipperton Fracture Zone . Kingston: International Seabed Authority. ISA Technical Study, Vol. 6, p. 105.ISA, "A geological model of polymetallic nodule deposits in the Clarion-Clipperton Fracture Zone," ISA, Tech...
The so-called “manganese nodule belt” (Halbach et al., 1988) extends along the sublatitudinal direction over 5000 km in the Pacific Ocean between the Clarion and Clipperton fracture zones (from 116° to 155° W) and has a width of about 1000 km (from 5° to 15° N). The...
Clarion-Clipperton ZoneGraphoglyptidPaleodictyon is an important trace fossil characterised by a regular hexagonal structure and typical of ancient deep-ocean habitats as far back as the Ordovician. It is represented in modern deep-sea settings by Paleodictyon nodosum, known from the Mid-Atlantic ...