{"_buckets": {"deposit": "b8698ca6-00f6-4c5a-8538-888c91ba2040"}, "_deposit": {"id": "33502", "owner": "1", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "33502"}, "status": "published"}, "_oai": {"id": "oai:repository.dl.itc.u-tokyo.ac.jp:00033502", "sets": []}, "author_link": ["130847", "130848", "130849"], "item_4_alternative_title_1": {"attribute_name": "\u305d\u306e\u4ed6\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "\u5730\u7403\u71b1\u5b66 \u7b2c21\u5831 : \u6771\u592a\u5e73\u6d0b\u6d77\u57df\u306e\u5730\u6bbb\u71b1\u6d41\u91cf"}]}, "item_4_biblio_info_7": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1967-08-25", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "2", "bibliographicPageEnd": "393", "bibliographicPageStart": "375", "bibliographicVolumeNumber": "45", "bibliographic_titles": [{"bibliographic_title": "\u6771\u4eac\u5927\u5b78\u5730\u9707\u7814\u7a76\u6240\u5f59\u5831 = Bulletin of the Earthquake Research Institute, University of Tokyo"}]}]}, "item_4_description_13": {"attribute_name": "\u30d5\u30a9\u30fc\u30de\u30c3\u30c8", "attribute_value_mlt": [{"subitem_description": "application/pdf", "subitem_description_type": "Other"}]}, "item_4_description_5": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "One hundred and ninety-seven new heat-flow measurements taken by Scripps Institution of Oceanography in the east Pacific Ocean off the coast of North and Central America are presented. These and three hundred and sixty-seven previous measurements taken in the eastern Pacific Ocean, east of 140\u00b0W and between 60\u00b0N and 10\u00b0S are used to describe the regional pattern of the area. A contour map is presented. The eastern Pacific Ocean is divided into three distinct regions: the area north of 25\u00b0N comprising the Mason-Raff magnetic lineations, a second region comprising the California Seamount Province, the East Pacific Rise, the Gulf of California, and the eastern Pacific Ocean basin, and finally a third area east of 100\u00b0W which encompasses the Middle America Trench, the Cocos, Galapagos and Carnegie ridges, the Galapagos Platform and the Guatemala Basin. An analysis is made of the heat-flow measurements in each area. This analysis shows that in the second and third regions, large areas exist having an average outward flow of heat greater than 3.0\u03bccal/cm2/sec, the oceanic average is 1.58\u03bccal/cm2/sec (Lee and Uyeda, 1965). These areas which are adjacent to equally large areas of subnormal heat-flow are in striking contrast with the uniformity of heat-flow which has recently been discovered in the northwest Pacific basin and seems to be typical of other ocean basins. It is unlikely that the distribution of these areas of high and low flow east of the East Pacific Rise can be explained by large-scale thermal convection cells in the mantle.", "subitem_description_type": "Abstract"}, {"subitem_description": "\u30b9\u30af\u30ea\u30d6\u30b9\u6d77\u6d0b\u7814\u7a76\u6240\u3067\u306f,\u5317\u7c73,\u4e2d\u7c73\u6c96\u306b\u65b0\u305f\u306b197\u70b9\u306e\u6d77\u6d0b\u5e95\u5730\u6bbb\u71b1\u6d41\u91cf\u306e\u6e2c\u5b9a\u3092\u884c\u306a\u3044,\u5f93\u6765\u306e367\u70b9\u3092\u52a0\u3048\u3066,\u897f\u7d4c140\u00b0\u4ee5\u6771\u306e\u5357\u7def10\u00b0\u3088\u308a\u5317\u7def60\u00b0\u306b\u304a\u3088\u3076\u6d77\u57df\u306b\u304a\u3044\u3066\u5730\u6bbb\u71b1\u6d41\u91cf\u306e\u5730\u57df\u7684\u5206\u5e03\u3092\u541f\u5473\u3057\u305f.\u3053\u306e\u7d50\u679c,\u6771\u592a\u5e73\u6d0b\u306f, 1) \u5317\u7def25\u00b0\u4ee5\u5317\u306eMason-Raff\u306e\u5730\u78c1\u6c17\u7e1e\u72b6\u5e2f\u3092\u542b\u3080\u6d77\u57df, 2)\u30ab\u30eb\u30d5\u30a9\u30eb\u30cb\u30a2\u6d77\u5c71\u5730\u5e2f,\u6771\u592a\u5e73\u6d0b\u6d77\u5dba,\u30ab\u30eb\u30d5\u30a9\u30eb\u30cb\u30a2\u6e7e,\u6771\u592a\u5e73\u6d0b\u6d77\u76c6\u7b49\u3092\u542b\u3080\u6d77\u57df, 3)\u4e2d\u592e\u30a2\u30e1\u30ea\u30ab\u6d77\u6e9d,\u30b3\u30b3,\u30ac\u30e9\u30d1\u30b4\u30b9,\u30ab\u30fc\u30cd\u30ae\u30fc\u306e\u6d77\u5dba,\u30ac\u30c6\u30de\u30e9\u6d77\u76c6\u306a\u3069\u306e\u897f\u7d4c100\u00b0\u4ee5\u6771\u306e\u6d77\u57df\u306e3\u6d77\u57df\u306b\u5927\u5225\u3055\u308c\u308b. 2), 3)\u306e\u6d77\u57df\u306b\u304a\u3044\u3066\u306f,\u3044\u304f\u3064\u3082\u306e\u5927\u304d\u306a\u9762\u7a4d\u3092\u5360\u308b\u5e73\u57473.0\u03bccal/cm2sec\u4ee5\u4e0a\u306e\u9ad8\u71b1\u6d41\u91cf\u5e2f\u304c,\u540c\u898f\u6a21\u306e\u4e16\u754c\u5e73\u5747(1.58\u03bccal/cm2sec)\u4ee5\u4e0b\u306e\u4f4e\u6d41\u91cf\u5e2f\u3068\u96a3\u63a5\u3057\u3066\u5b58\u5728\u3057\u3066\u304a\u308a,\u5317\u897f\u592a\u5e73\u6d0b\u6d77\u76c6\u7b49\u306e\u4ed6\u306e\u6df1\u6d77\u76c6\u306b\u304a\u3051\u308b\u4e00\u69d8\u306a\u5730\u6bbb\u71b1\u6d41\u91cf\u306e\u5206\u5e03\u3068\u8457\u3057\u3044\u5bfe\u7167\u3092\u306a\u3057\u3066\u3044\u308b.\u6771\u592a\u5e73\u6d0b\u6d77\u5dba\u4ee5\u6771\u306e\u3053\u306e\u9ad8\u4f4e\u71b1\u6d41\u91cf\u306e\u5206\u5e03\u3092\u5927\u898f\u6a21\u306a\u30de\u30f3\u30c8\u30eb\u71b1\u5bfe\u6d41\u6838\u3067\u8aac\u660e\u3059\u308b\u3053\u3068\u306f\u56f0\u96e3\u3067\u3042\u308b\u3088\u3046\u306b\u601d\u308f\u308c\u308b.", "subitem_description_type": "Abstract"}]}, 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"item_title": "Studies of the Thermal State of the Earth. The 21st Paper : Heat-Flow, Eastern Pacific", "item_titles": {"attribute_name": "\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_title": "Studies of the Thermal State of the Earth. The 21st Paper : Heat-Flow, Eastern Pacific", "subitem_title_language": "en"}]}, "item_type_id": "4", "owner": "1", "path": ["80/4535/4927/4933", "9/504/4538/4929/4934"], "permalink_uri": "https://doi.org/10.15083/0000033502", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2008-05-30"}, "publish_date": "2008-05-30", "publish_status": "0", "recid": "33502", "relation": {}, "relation_version_is_last": true, "title": ["Studies of the Thermal State of the Earth. The 21st Paper : Heat-Flow, Eastern Pacific"], "weko_shared_id": -1}