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我国南海历史性水域线的地质特征 被引量:6
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作者 夏戡原 夏综万 +1 位作者 赵明辉 孙珍 《海洋学报》 CAS CSCD 北大核心 2014年第5期77-89,共13页
40a的海洋地质、地球物理实测研究表明,九段线不仅是显示我国南海主权的历史性水域线,而且总体上也是南海与东部、南部和西部陆区及岛区的巨型地质边界线。根据实测数据,本文将从地质成因、来源、演化的角度论述此南海历史性水域线... 40a的海洋地质、地球物理实测研究表明,九段线不仅是显示我国南海主权的历史性水域线,而且总体上也是南海与东部、南部和西部陆区及岛区的巨型地质边界线。根据实测数据,本文将从地质成因、来源、演化的角度论述此南海历史性水域线的合理性。主要结论包括:历史性水域线的东段在地形上基本与马尼拉海沟一致,海沟西侧为南海中央海盆洋壳区,东侧为菲律宾群岛。根据国际地质研究的资料,菲律宾群岛始新世以前位于较偏南的纬度,后来于中晚中新世(距今16~10Ma)仰冲于南海中央海盆之上,因此菲律宾群岛是一个外来群岛。而黄岩岛在马尼拉海沟以西,是中央海盆洋壳区的一个岛礁,与菲律宾群岛成因不同。南海历史性水域线的南段在地形上基本与南沙海槽一致,伴随南沙地块由北部陆缘向南裂离,古南海洋壳沿此海槽以南俯冲至加里曼丹岛陆壳之下,因此南沙地块与加里曼丹陆块为两个来历不同的地块。南海历史性水域线西段的分布在地形上与越东巨型走滑断裂带基本一致,可能与西沙地块、中沙地块、南沙地块从南海北部陆缘向南滑移有关。南沙地块北缘陡直的正断层结构,突显中央海盆是拉裂形成,其基底和中新生代地层与北部珠江口盆地的地层结构可以对比,说明南沙岛礁原属我国华南大陆南缘,后因南海的形成裂离至现今的位置。 展开更多
关键词 历史性水域线 地质演化 地质来源 马尼拉海沟 南沙海槽 越东断裂
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某小矿体地质特征及成因探讨
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作者 周志辉 《西部探矿工程》 CAS 2004年第8期83-85,共3页
外围小矿体均赋存于泥盆系生物礁灰岩中 ,呈脉状产出 ,矿床类型为锡石—多金属硫化物矿床 ,成矿物质主要来源于花岗岩 ,部分来源于泥盆系地层。
关键词 小矿体 地质特征:物质来源 成矿模式 矿床成因
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Banana-dairy Small Scale Farming System for the North Rift Region of Kenya
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作者 Francesca Naliaka Lusweti Zaddock MacOsore Nelson W. Khisa 《Journal of Life Sciences》 2011年第6期466-471,共6页
Feeding costs could be reduced by use of alternative energy and protein sources. Leguminous trees remain green through the dry season, serving as a crude protein bank besides improving soil fertility through nitrogen ... Feeding costs could be reduced by use of alternative energy and protein sources. Leguminous trees remain green through the dry season, serving as a crude protein bank besides improving soil fertility through nitrogen fixation, nutrients recycling and stabilising soil on terraces. Some Kenyan farmers intercrop bananas with forages to cope with the perennial feed shortages. A simulation model assumed a family of six (husband, wife and four children) owning one cow producing 15 kg milk per day, living on 0.4 ha of land. Bananas grown on 0.36 ha in alleys of alternating rows ofLeucaena diversifolia and Calliandra calothyrses, intercropped with Guinea grass (Panicum maximum) and Desmodium uncinatum. Napier (Pennisetum purpureum) was planted in the alleys as a pure stand on 0.08 ha. Model analysis showed the household had adequate energy and protein all the year and was financially secured, with income exceeding routine expenditure. There were positive balances for nitrogen and phosphorus, but potassium application was required. A replica of the model was then tested. 展开更多
关键词 INTEGRATION BANANA fodder trees forage crops dairy.
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Geochemical characteristics and geological significance of Cretaceous phonotephrite from the Mid-Pacific Mountains 被引量:1
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作者 Shuangshuang CHEN Jiaqi LIU 《Science China Earth Sciences》 SCIE EI CAS CSCD 2018年第6期745-764,共20页
Systematic analyses were conducted including the petrographic features, major and trace elements, Sr and Nd isotopic compositions, and mineral structure and compositions of whole rocks. Mid-Pacific Mountain volcanic r... Systematic analyses were conducted including the petrographic features, major and trace elements, Sr and Nd isotopic compositions, and mineral structure and compositions of whole rocks. Mid-Pacific Mountain volcanic rocks are mainly phonotephrite with a porphyritic texture. Phenocrysts are mainly composed of Ca-rich plagioclase, clinopyroxene and nepheline.These volcanic rocks are significantly rich in large-ion lithophile and light rare earth elements, without obvious Eu anomalies(δEu=0.99–1.03), and with relatively enriched^(87) Sr/^(86) Sr(0.703829–0.704313) and^(143) Nd/^(144) Nd isotopic ratios(0.512857–0.512871), suggesting that they have similar but more enriched features than the OIB magmatic source. These volcanic rocks may originate from relatively deep magma source with the existence of spinel-garnet Iherzolites, and have undergone partial melting at a low degree of 1–3%. In addition, The residual Nb-Ta minerals(such as sphene, rutile, perovskite) may remain in the mantle source, and the magma components have undergone metasomatism by carbonate melt/fluid or alkali-rich fluid, causing high contents of incompatible elements and significant loss of Nb, Ta and Ti in these volcanic rocks. There are many similarities between the phonotephrites in the Mid-Pacific Mountain and the volcanic rocks in the Line Islands based on the tectonic settings and the geochemical characteristics. We thus speculate that Site 313 volcanic rocks in the Mid-Pacific Mountain is most likely to be a continuation of the Line Islands. 展开更多
关键词 Phonotephrite OIB-type mantle source Carbonatite metasomatism Line Islands Mid-Pacific Mountain
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