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Mass transport, reaction and deformation at slab-mantle interface induced by H2O-CO2 fluids
(H2O-CO2\u6d41\u4f53\u306b\u8d77\u56e0\u3059\u308b\u30b9\u30e9\u30d6\u30fc\u30de\u30f3\u30c8\u30eb\u5883\u754c\u306b\u304a\u3051\u308b\u7269\u8cea\u79fb\u52d5\u3001\u53cd\u5fdc\u3001\u5909\u5f62)<\/p>\n\n\n\n
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Data-Driven Analyses of Element Transfer within Oceanic Crust During Fluid-Rock Interactions at Seafloor and Subduction Plate Interface
(\u6d77\u6d0b\u5e95\u30fb\u6c88\u307f\u8fbc\u307f\u30d7\u30ec\u30fc\u30c8\u5883\u754c\u306b\u304a\u3051\u308b \u5ca9\u77f3-\u6d41\u4f53\u76f8\u4e92\u4f5c\u7528\u306b\u4f34\u3046\u5143\u7d20\u79fb\u52d5\u306e\u30c7\u30fc\u30bf\u99c6\u52d5\u578b\u89e3\u6790)<\/p>\n\n\n\n2023\u5e74\u5ea6<\/h2>\n\n\n\n
\u5b66\u58eb\u8ad6\u6587<\/h4>\n\n\n\n
MgO\u306e\u6c34\u548c\u81a8\u5f35\u53cd\u5fdc\u306b\u304a\u3051\u308b\u6d78\u900f\u7387\u3068\u53cd\u5fdc\u8a98\u8d77\u5fdc\u529b\u306e\u540c\u6642\u8a08\u6e2c<\/p>\n\n\n\n
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\u6d77\u5e95\u71b1\u6c34\u5674\u51fa\u5b54\u306b\u304a\u3051\u308b\u30c1\u30e0\u30cb\u30fc\u7d2f\u5e2f\u69cb\u9020\u306e\u767a\u9054 \u3068\u71b1\u96fb\u5909\u63db\u6a5f\u80fd\u306e\u767a\u73fe<\/p>\n\n\n\n\u535a\u58eb\u8ad6\u6587<\/h4>\n\n\n\n
Interplay of Fluid Infiltration, Reaction and Fracturing in the Oceanic Lithosphere<\/p>\n\n\n\n2022\u5e74\u5ea6<\/h2>\n\n\n\n
\u5b66\u58eb\u8ad6\u6587<\/h4>\n\n\n\n
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\u6d77\u5e95\u71b1\u6c34\u9271\u5e8a\u306e\u5f62\u6210\u306b\u4f34\u3046\u77f3\u82f1\u7c92\u5b50\u306e\u751f\u6210\u30d7\u30ed\u30bb\u30b9<\/p>\n\n\n\n
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\u5b66\u58eb\u8ad6\u6587<\/h4>\n\n\n\n
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\u6a5f\u68b0\u5b66\u7fd2\u306b\u3088\u308b\u7384\u6b66\u5ca9\u8cea\u5909\u6210\u5ca9\u306e\u539f\u5ca9\u7d44\u6210\u63a8\u5b9a\u3068\u7269\u8cea\u79fb\u52d5\u89e3\u6790<\/p>\n\n\n\n2020\u5e74\u5ea6<\/h2>\n\n\n\n
\u5b66\u58eb\u8ad6\u6587<\/h4>\n\n\n\n
<\/strong>\u5730\u6bbb\u306e\u4f53\u7a4d\u81a8\u5f35\u53cd\u5fdc\u306b\u3088\u308b\u6d78\u900f\u7387\u4e0a\u6607\u30e1\u30ab\u30cb\u30ba\u30e0\u306b\u95a2\u3059\u308b\u5b9f\u9a13\u7684\u7814\u7a76<\/p>\n\n\n\n
<\/strong>\u6d77\u5e95\u71b1\u6c34\u5674\u51fa\u5b54\u306b\u304a\u3051\u308b\u9271\u7269\u7c92\u5b50\u306e\u5f62\u6210\u30fb\u904b\u642c\u904e\u7a0b\u306b\u95a2\u3059\u308b\u5b9f\u9a13\u7684\u7814\u7a76<\/p>\n\n\n\n
<\/strong>\u9ad8\u6e29\u30fb\u30a2\u30eb\u30ab\u30ea\u74b0\u5883\u4e0b\u306b\u304a\u3051\u308b\u30de\u30f3\u30c8\u30eb\u304b\u3093\u3089\u3093\u5ca9\u306e\u86c7\u7d0b\u5ca9\u5316\u3068\u78c1\u9244\u9271\u751f\u6210\u306b\u95a2\u3059\u308b\u7814\u7a76<\/p>\n\n\n\n\u4fee\u58eb\u8ad6\u6587<\/h4>\n\n\n\n
<\/strong>\u71b1\u529b\u5b66\u30c7\u30fc\u30bf\u306e\u62e1\u5f35\u306b\u57fa\u3065\u304f\u8d85\u81e8\u754c\u5730\u71b1\u30b7\u30b9\u30c6\u30e0\u306b\u304a\u3051\u308b\u9271\u7269\u30fc\u6d41\u4f53\u5e73\u8861\u30e2\u30c7\u30ea\u30f3\u30b0<\/p>\n\n\n\n
<\/strong>Enhanced fluid infiltration by reaction-induced fracturing within the oceanic lithosphere<\/p>\n\n\n\n2019\u5e74\u5ea6<\/h2>\n\n\n\n
\u5b66\u58eb\u8ad6\u6587<\/h4>\n\n\n\n
<\/strong>\u591a\u6b21\u5143\u5730\u7403\u79d1\u5b66\u30c7\u30fc\u30bf\u306e\u7d71\u8a08\u89e3\u6790\u306b\u3088\u308b\u539f\u5ca9\u69cb\u6210\u8b58\u5225\u3068\u6d41\u4f53\u53cd\u5fdc<\/p>\n\n\n\n\u535a\u58eb\u8ad6\u6587<\/h4>\n\n\n\n
<\/strong>Mass Transport during Metamorphic Processes of the Khantaishir Ophiolite, Western Mongolia<\/p>\n\n\n\n2018\u5e74\u5ea6<\/h2>\n\n\n\n
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<\/strong>\u8d85\u81e8\u754c\u6761\u4ef6\u3078\u306e\u6eb6\u5b58\u7a2e\u306e\u71b1\u529b\u5b66\u30c7\u30fc\u30bf\u306e\u62e1\u5f35\u3068\u5b9f\u9a13\u7684\u691c\u8a3c<\/p>\n\n\n\n
<\/strong>\u6d77\u6d0b\u5e95\u5c64\u72b6\u6591\u308c\u3044\u5ca9\u306e\u52a0\u6c34\u53cd\u5fdc\u306b\u4f34\u3046\u304d\u88c2\u30cd\u30c3\u30c8\u30ef\u30fc\u30af\u5f62\u6210\u306b\u95a2\u3059\u308b\u6570\u5024\u30e2\u30c7\u30ea\u30f3\u30b0<\/p>\n\n\n\n\u4fee\u58eb\u8ad6\u6587<\/h4>\n\n\n\n
<\/strong>Migration and Reaction of Magmatic Fluids Related to Granitic Pegmatite Complex in Kinkasan Island, NE Japan<\/p>\n","protected":false},"excerpt":{"rendered":"