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CONTINENTAL ROCKS IN THE INDIAN OCEAN
Takao YANO*, Boris I. VASILIEV**, Dong R. CHOI***, Seiko MIYAGI****,
Alexander A. GAVRILOV** and Hisao ADACHI*****
* Department of Environment Science, Faculty of Regional Science, Tottori Univ., Tottori, 680-855, Japan.
** Pacific Oceanological Institute, Far East Branch, Russian Academy of Science, Vladivostok, 690041, Russia.
*** Raax Australia Pty Ltd., 6 Mann Place, Higgins, ACT 2615, Australia.
**** Tokyo Metropolitan Kitazono Senior High School, Itabashi-ku, Tokyo, 173-0004, Japan. ****** Tokyo Metropolitan Nerima Senior High School, Nerima-ku, Tokyo, 179-8908, Japan.
Abstract: This paper reviews the occurrence of continental rocks at 32 localities in the Indian Ocean. Almost all of them were found in rises, plateaus, and ridges situated in the marginal ocean basins.
In the world oceans – the Atlantic, Indian and Pacific Oceans – ancient continental rocks have been discovered at a total of 78 localities. Type A rocks (continental rocks located in continental margins deeper than the ocean-floor depth) indicate that part of the continent has submerged and turned to ocean floor – a phenomenon recognized by all proposed ocean-formation hypotheses. Type B rocks (continental rocks located in mid-oceanic ridges and ocean basins) and Type C rocks (rocks characterized by continental geochemical signatures) located in mid-oceanic ridges and ocean basins are incompatible with the hypothesis of ocean-floor spreading, but they provide powerful supporting evidence for the oceanization and microexpansion hypotheses.
The two gigantic ring structures – the Dupal anomaly belt and the circum-Pacific mobile belt – indicate that the Earth’s mantle is rather inhomogeneous in chemical composition and is not so active and fluidal as generally believed. The keys to future ocean-formation debates are Type B and C rocks. To understand the ocean-formation processes, the thermal and compositional inhomogeneity and low fluidity of the mantle are important constraints.
Keywords: continental rocks, Indian Ocean, ocean-floor spreading, oceanization, microexpansion, Dupal anomaly, circum-Pacific mobile belt, Earth’s dichotomy
The standard view has been that the inner core is freezing all over and growing out progressively, but it appears that there are regions where the core is actually melting. The net flow of heat from core to mantle ensures that there's still overall freezing of outer core material and it's still growing over time, but by no means is this a uniform process.
Extremely windy or stormy in places with very strong and blustery southwest to west winds gusting to between 80 and 100 km/h generally, but up to 140 km/h in exposed hilly and coastal areas of Ulster and Connacht.
At the same time, Owen also introduced an ingenious idea: "Are the pressure and heat in the interior of the Earth enough to maintain a plasma core? They probably are, and the solid nickel-iron core of the textbooks may be a myth". According to the transmission of seismic waves through the Earth's core and the composition of meteorites, it had previously been thought that the inner core was solid, composed of nickel, iron and probably sulphur. The outer core was assumed to be molten. Owen explains that "the behaviour of waves passing through a plasma core would be similar to that in a solid iron-sulphur core".
He suggests that if the inner core is plasma there is a potential for expansion when the core changes from a plasma into an atomic state. The Earth's outer core may be molten because it has already changed into its atomic state. (This author adds that an explosion potential would also be present if the gravity envelope had been broken by an impact catastrophe.)
bye bye plate tectonics