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斧山
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     PETROGENESIS OF THE FUSHAN ALKALI BASALTS AND THEIR PERIDOTITIC INCLUSIONS FROM DANGTU, ANHUI PROVINCE
     斧山碱性玄武岩及其橄榄岩类包体的成因岩石学
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     Fusible components are vario- us with degree of partial melting. Mineralogical compositions of Ihe- rzolite also indicate this point. The calculated results ef pressure and temperture for Iherzolites are 1040-1216℃ and 25-32 kb which indicate that inclusion have been formde at depth about 70 100Km.
     通过包体矿物组合、成分等分析,表明斧山橄榄岩包体属富集易熔组份的饱满型包体,估算矿物平衡结晶温度为1040—1216℃,压力为25—32kb,推测包体来源深度为70—100公里。
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     Mountain King In The World
     天下第一
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     WU MENG MOUNTAIN
     乌蒙
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     PETROGENESIS OF THE FUSHAN ALKALI BASALTS AND THEIR PERIDOTITIC INCLUSIONS FROM DANGTU, ANHUI PROVINCE
     碱性玄武岩及其橄榄岩类包体的成因岩石学
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     CLEAVERS IN CHINA
     中国的薄刃
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The Fushan is known as an early pleistoceno volcano which consists of basanites and olivine-nephelinites. Lherzolite inclusions and megac- rystals of garnet, augite and Ti-phlogopite occur in these rocks. Lherzoli- tes have unequal-grainned, porphyroclasic, unequal-blastic, and partial melting texture. The last three types are dominant. Chemical compositions of the basanite and nephelinite are charac- terized by rich-incompatible elements K, P, Ti and higher Na_2O and Al_2O_3/CaO ratio. These basalts show rapidly...

The Fushan is known as an early pleistoceno volcano which consists of basanites and olivine-nephelinites. Lherzolite inclusions and megac- rystals of garnet, augite and Ti-phlogopite occur in these rocks. Lherzoli- tes have unequal-grainned, porphyroclasic, unequal-blastic, and partial melting texture. The last three types are dominant. Chemical compositions of the basanite and nephelinite are charac- terized by rich-incompatible elements K, P, Ti and higher Na_2O and Al_2O_3/CaO ratio. These basalts show rapidly fractioctionated transition metal and REE distribution patterns. Above mentioned facts indicate the basanite and nephelinite are products of low melting of mantle- peridotites (7%). Their M value is lower (53-66) which may be suggest primary basaltic magma undergone fractionation at high pressure. Lherzolites are enriched in fusible components and have lower 100Mg/Mg+TFe ratio. Transition metal and REE have slightly distribu- tion patterns belonging to fertile mantle. Fusible components are vario- us with degree of partial melting. Mineralogical compositions of Ihe- rzolite also indicate this point. The calculated results ef pressure and temperture for Iherzolites are 1040-1216℃ and 25-32 kb which indicate that inclusion have been formde at depth about 70 100Km.

通过全岩和矿物化学、过渡金属以及REE的分配图式等分析研究,表明斧山玄武岩是原始地幔橄榄岩经受高压分离作用的产物。通过包体矿物组合、成分等分析,表明斧山橄榄岩包体属富集易熔组份的饱满型包体,估算矿物平衡结晶温度为1040—1216℃,压力为25—32kb,推测包体来源深度为70—100公里。

 
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