Nicaise Blaise Tchuimegnié Ngongang, Merlin Patrick Njombie Wagsong, F. Owono, I. Badriyo, P. Essomba, Nathalie Love Ngongang Tchikankou, Dieudonné Youmen, Pierre Kamgang, G. Chazot
{"title":"西非巴方及其周边(喀麦隆火山岩线)新生代板内碱性火山岩的矿物学及岩浆作用","authors":"Nicaise Blaise Tchuimegnié Ngongang, Merlin Patrick Njombie Wagsong, F. Owono, I. Badriyo, P. Essomba, Nathalie Love Ngongang Tchikankou, Dieudonné Youmen, Pierre Kamgang, G. Chazot","doi":"10.4236/ojg.2021.116013","DOIUrl":null,"url":null,"abstract":"Alkaline \nbasalts of Bafang and its environs are consisted of feldspars, olivines, pyroxenes \nand oxides which appear as phenocrysts, microphenocrysts and microcrysts. \nFeldspars are plagioclases (An67.97-15.84Ab69.19-30.43Or20.59-1.51) \nand anorthoclases (Ab68.11-61.20Or33.87-20.91An10.98-4.93). \nPlagioclases are the most abundant amount these feldspars. Anorthoclases appear \nonly in mugearite (BAF 3 and BAF 37) the most differentiated of the studied alkaline-basalts. \nIn High Magnesian basalt, (HMg-B) plagioclases are labradorites (An67.97-59.30Ab38.74-30.43Or2.75-1.60) \nand sanidine (An45.44-31.82Ab62.66-51.79Or5.52-2.77), \nwhereas in Low Magnesian basalt (LMg-B) there are labrador (An67.4.75-51.96Ab44.98-33.72Or3.06-1.51), \nandesine (An45.44-31.82Ab62.66-51.79Or5.52-2.77), \noligoclase (An26.65-15.84Ab69.19-63.57Or20.59-8.55) \nand anarthoclase (Ab68.11-61.20Or33.87-20.91An10.98-4.93). \nOlivines are magnesian (Fo86.7-50.1) and ferriferous (Fo48.8-37.8). \nIn HMg-B, olivine are only magnesian. These olivines are \nchrysolites and hyalositerite. In LMg-B, olivines are magnesian and ferriferous with the predominance of ferriferous. \nThey are chrysolites, hyalositerite and hortonolite. Pyroxenes are Ca, Mg and \nFe clinopyroxenes. There are diopsides (Wo51.94-45.02En44.41-33.16Fs16.42-10.70) \nand augites (Wo44.88-43.64En41.03-37.04Fs18.25-14.43). \nOxides are magnetites represented by ulvospinel (Usp90-75Sp2-7Mt5-23). \nFractionation of ferromagnesian minerals (opaque oxide, olivine and pyroxene) \nis the main differentiation process. Two stages of fractional crystallization \ncan be distinguished: the first stage comes with basanites and the second with \nhawaiites to mugearites. Chemical compositions of phenocrystals in studied basaltics \nlavas record signatures of magma recharge by pulsatory intrusions of new magma \ninto the existing magma reservoir before the eruptions.","PeriodicalId":63246,"journal":{"name":"地质学期刊(英文)","volume":" ","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2021-06-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"Mineralogy and Magmatic Processes of Cenozoic Intraplate Alkaline Volcanic Rocks of Bafang and Its Environs (Cameroon Volcanic Line, West Africa)\",\"authors\":\"Nicaise Blaise Tchuimegnié Ngongang, Merlin Patrick Njombie Wagsong, F. Owono, I. Badriyo, P. Essomba, Nathalie Love Ngongang Tchikankou, Dieudonné Youmen, Pierre Kamgang, G. Chazot\",\"doi\":\"10.4236/ojg.2021.116013\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Alkaline \\nbasalts of Bafang and its environs are consisted of feldspars, olivines, pyroxenes \\nand oxides which appear as phenocrysts, microphenocrysts and microcrysts. \\nFeldspars are plagioclases (An67.97-15.84Ab69.19-30.43Or20.59-1.51) \\nand anorthoclases (Ab68.11-61.20Or33.87-20.91An10.98-4.93). \\nPlagioclases are the most abundant amount these feldspars. Anorthoclases appear \\nonly in mugearite (BAF 3 and BAF 37) the most differentiated of the studied alkaline-basalts. \\nIn High Magnesian basalt, (HMg-B) plagioclases are labradorites (An67.97-59.30Ab38.74-30.43Or2.75-1.60) \\nand sanidine (An45.44-31.82Ab62.66-51.79Or5.52-2.77), \\nwhereas in Low Magnesian basalt (LMg-B) there are labrador (An67.4.75-51.96Ab44.98-33.72Or3.06-1.51), \\nandesine (An45.44-31.82Ab62.66-51.79Or5.52-2.77), \\noligoclase (An26.65-15.84Ab69.19-63.57Or20.59-8.55) \\nand anarthoclase (Ab68.11-61.20Or33.87-20.91An10.98-4.93). \\nOlivines are magnesian (Fo86.7-50.1) and ferriferous (Fo48.8-37.8). \\nIn HMg-B, olivine are only magnesian. These olivines are \\nchrysolites and hyalositerite. In LMg-B, olivines are magnesian and ferriferous with the predominance of ferriferous. \\nThey are chrysolites, hyalositerite and hortonolite. Pyroxenes are Ca, Mg and \\nFe clinopyroxenes. There are diopsides (Wo51.94-45.02En44.41-33.16Fs16.42-10.70) \\nand augites (Wo44.88-43.64En41.03-37.04Fs18.25-14.43). \\nOxides are magnetites represented by ulvospinel (Usp90-75Sp2-7Mt5-23). \\nFractionation of ferromagnesian minerals (opaque oxide, olivine and pyroxene) \\nis the main differentiation process. Two stages of fractional crystallization \\ncan be distinguished: the first stage comes with basanites and the second with \\nhawaiites to mugearites. Chemical compositions of phenocrystals in studied basaltics \\nlavas record signatures of magma recharge by pulsatory intrusions of new magma \\ninto the existing magma reservoir before the eruptions.\",\"PeriodicalId\":63246,\"journal\":{\"name\":\"地质学期刊(英文)\",\"volume\":\" \",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2021-06-08\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"地质学期刊(英文)\",\"FirstCategoryId\":\"1089\",\"ListUrlMain\":\"https://doi.org/10.4236/ojg.2021.116013\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"地质学期刊(英文)","FirstCategoryId":"1089","ListUrlMain":"https://doi.org/10.4236/ojg.2021.116013","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Mineralogy and Magmatic Processes of Cenozoic Intraplate Alkaline Volcanic Rocks of Bafang and Its Environs (Cameroon Volcanic Line, West Africa)
Alkaline
basalts of Bafang and its environs are consisted of feldspars, olivines, pyroxenes
and oxides which appear as phenocrysts, microphenocrysts and microcrysts.
Feldspars are plagioclases (An67.97-15.84Ab69.19-30.43Or20.59-1.51)
and anorthoclases (Ab68.11-61.20Or33.87-20.91An10.98-4.93).
Plagioclases are the most abundant amount these feldspars. Anorthoclases appear
only in mugearite (BAF 3 and BAF 37) the most differentiated of the studied alkaline-basalts.
In High Magnesian basalt, (HMg-B) plagioclases are labradorites (An67.97-59.30Ab38.74-30.43Or2.75-1.60)
and sanidine (An45.44-31.82Ab62.66-51.79Or5.52-2.77),
whereas in Low Magnesian basalt (LMg-B) there are labrador (An67.4.75-51.96Ab44.98-33.72Or3.06-1.51),
andesine (An45.44-31.82Ab62.66-51.79Or5.52-2.77),
oligoclase (An26.65-15.84Ab69.19-63.57Or20.59-8.55)
and anarthoclase (Ab68.11-61.20Or33.87-20.91An10.98-4.93).
Olivines are magnesian (Fo86.7-50.1) and ferriferous (Fo48.8-37.8).
In HMg-B, olivine are only magnesian. These olivines are
chrysolites and hyalositerite. In LMg-B, olivines are magnesian and ferriferous with the predominance of ferriferous.
They are chrysolites, hyalositerite and hortonolite. Pyroxenes are Ca, Mg and
Fe clinopyroxenes. There are diopsides (Wo51.94-45.02En44.41-33.16Fs16.42-10.70)
and augites (Wo44.88-43.64En41.03-37.04Fs18.25-14.43).
Oxides are magnetites represented by ulvospinel (Usp90-75Sp2-7Mt5-23).
Fractionation of ferromagnesian minerals (opaque oxide, olivine and pyroxene)
is the main differentiation process. Two stages of fractional crystallization
can be distinguished: the first stage comes with basanites and the second with
hawaiites to mugearites. Chemical compositions of phenocrystals in studied basaltics
lavas record signatures of magma recharge by pulsatory intrusions of new magma
into the existing magma reservoir before the eruptions.