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Studies show that the average ratio of w/w(P2O5)(1.62) of phosphates in submarine guyots is the same as that of w/w(P2O5)（1.621）of carbonate-fluorapatite, but is obviously different from that of w/w(P2O5)（1.318）of fluorine_carbonate, suggesting that the phosphates from northwestern Pacific are species of carbonate_fluorapatite.Three types of microneedle-microcolumnar, microgranular and microcryptocrystalline carbonate_fluorapatite with different abundances have been found.
海山磷酸盐的平均化学成分w/w(P2O5)（1.62）与碳氟磷灰石的w/w(P2O5)（1.621）几乎一致，而与氟磷灰石的w/w(P2O5)（1.318）相差甚远，表明海山磷酸盐为碳氟磷灰石，其形态主要有针状_柱状微晶碳氟磷灰石、粒状微晶碳氟磷灰石及显微隐晶质碳氟磷灰石3种类型，它们在分布丰度上存在差异。
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Many guyots now lie below the surface.
很多平顶海山现在是在海面以下。
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The web site provides a database of species that were collected from underwater seamounts, guyots, and ridges, along with sampling procedure information.
该数据库收录的范围包括水下海山、海底平顶山、海洋山脊等，目前拥有114座海山1600物种的7000多条记录，并且数据量也在不断增长更新。
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Geological features of phosphorates associated with cobalt_rich crusts on northwestern Pacific submarine guyots were studied systematically.
中文摘要：为了更好地认识大洋富钴结壳的成矿作用，作者对与其伴生的海山磷酸盐的产状、化学成分、种类及X射线衍射特征等进行了研究。
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The crystal constant of α has a range from 0.932 nm to 0.933 nm with an average of 0.933 nm. Various replacement and remnant structures show that the phosphorates in submarine guyots are mainly of replacement origin.
各种交代残余结构（交代角砾状结构、交代生物结构、交代凝灰结构、交代生物假象结构、交代填间结构等）表明，太平洋水下海山上的磷酸盐主要属交代成因。
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Guyots：平顶海山
Gyres 旋转 | Guyots 平顶海山 | Groundwater Quality 地下水质量