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A phlogopite-amphibole-plagioclase bearing websterite from Guinadji volcano (Adamawa Plateau, Northern Cameroon): evidence of a cumulate origin and crustal event Cover

A phlogopite-amphibole-plagioclase bearing websterite from Guinadji volcano (Adamawa Plateau, Northern Cameroon): evidence of a cumulate origin and crustal event

Open Access
|Dec 2025

Figures & Tables

Figure 1.

(a) Location of Adamawa plateau (red star) and other principal volcanic centers along the CVL (modified according to Nkouathio et al., 2008). Dashed lines are limits between the CVL segments: ocean, COB and continent. (b) Location map of the CVL. The principal geologic features of Africa (Congo Craton, CVL, East African Rift, Hoggar, Kalahari Craton, Tibesti, West African Craton) are indicated. COB, continental ocean boundary; CVL, Cameroon volcanic line.
(a) Location of Adamawa plateau (red star) and other principal volcanic centers along the CVL (modified according to Nkouathio et al., 2008). Dashed lines are limits between the CVL segments: ocean, COB and continent. (b) Location map of the CVL. The principal geologic features of Africa (Congo Craton, CVL, East African Rift, Hoggar, Kalahari Craton, Tibesti, West African Craton) are indicated. COB, continental ocean boundary; CVL, Cameroon volcanic line.

Figure 2.

Photomicrographs of the studied websterite. (a) Cumulative texture. (b) Interstitial phlogopite. (c) Edenite as rim around cpx. (d) Three aspects of opx. Dashed lines represent their triple junctions. hbi, host basalt infiltration, op, opaque minerals; Phl, phlogopite.
Photomicrographs of the studied websterite. (a) Cumulative texture. (b) Interstitial phlogopite. (c) Edenite as rim around cpx. (d) Three aspects of opx. Dashed lines represent their triple junctions. hbi, host basalt infiltration, op, opaque minerals; Phl, phlogopite.

Figure 3.

BSE images of the studied websterite. (a) Association phlogopite-amphibole-rutile. (b) Amphibolitization of clinopyoxene. (c) Amphibole elongated exsolution lamellae following clinopyroxene cleavage. (d) Plagioclase as intercumulus phase. (e) Image showing that amphibole and phlogopite are of metasomatic origin. (f) Clinopyroxene remants as inclusion in plagioclase. sul, sulfides.
BSE images of the studied websterite. (a) Association phlogopite-amphibole-rutile. (b) Amphibolitization of clinopyoxene. (c) Amphibole elongated exsolution lamellae following clinopyroxene cleavage. (d) Plagioclase as intercumulus phase. (e) Image showing that amphibole and phlogopite are of metasomatic origin. (f) Clinopyroxene remants as inclusion in plagioclase. sul, sulfides.

Figure 4.

Chondrite normalized REE (a) and spider diagram (b) of the Guinadji volcano websterite; normalization values are from Sun and McDonough (1989). REE, rare earth elements.
Chondrite normalized REE (a) and spider diagram (b) of the Guinadji volcano websterite; normalization values are from Sun and McDonough (1989). REE, rare earth elements.

Figure 5.

Pyroxene composition from the studied websterite plotted on the En-Wo-Fs ternary diagram after Morimoto et al. (1988).
Pyroxene composition from the studied websterite plotted on the En-Wo-Fs ternary diagram after Morimoto et al. (1988).

Figure 6.

Clino- and orthopyroxene mineral chemistry plots. (a) CaO (wt%) versus Mg# content of clinopyroxene, (b) Al2O3 versus Mg# for clinopyroxene, (c) CaO (wt%) versus Mg# content of clinopyroxene, (d) Al2O3 versus Mg# for clinopyroxene. Plagioclase-bearing olivine websterite from Serri et al. (1988), Layered websterite from Wilson and Chaumba (1997), Abyssal crustal cumulate pyroxenite after Dantas et al. (2007); Mantle websterites from Rogkala et al., 2017; Garnet websterites from Lu et al., 2018, Befang websterite from Tedonkenfack et al. (2021).
Clino- and orthopyroxene mineral chemistry plots. (a) CaO (wt%) versus Mg# content of clinopyroxene, (b) Al2O3 versus Mg# for clinopyroxene, (c) CaO (wt%) versus Mg# content of clinopyroxene, (d) Al2O3 versus Mg# for clinopyroxene. Plagioclase-bearing olivine websterite from Serri et al. (1988), Layered websterite from Wilson and Chaumba (1997), Abyssal crustal cumulate pyroxenite after Dantas et al. (2007); Mantle websterites from Rogkala et al., 2017; Garnet websterites from Lu et al., 2018, Befang websterite from Tedonkenfack et al. (2021).

Figure 7.

(a) Chemical composition of phlogopite on the Mg/(Fe + Mg) versus Altot classification diagram of Rieder et al. (1998). Red circles represent chemical compositions of phlogopite. (b) Amphibole classification diagram after Leake et al. (1997). The blue field represents amphiboles described by Pintér et al. (2015) and Njombie Wagsong et al. (2018). TFA, Tetra-Ferri-Annite; TFP, Tetra-Ferri-Phlogopite.
(a) Chemical composition of phlogopite on the Mg/(Fe + Mg) versus Altot classification diagram of Rieder et al. (1998). Red circles represent chemical compositions of phlogopite. (b) Amphibole classification diagram after Leake et al. (1997). The blue field represents amphiboles described by Pintér et al. (2015) and Njombie Wagsong et al. (2018). TFA, Tetra-Ferri-Annite; TFP, Tetra-Ferri-Phlogopite.

Figure 8.

Whole-rock CaO–Al2O3–MgO plot of the Guinadji volcano websterite (references of the fields after Selim et al., 2025).
Whole-rock CaO–Al2O3–MgO plot of the Guinadji volcano websterite (references of the fields after Selim et al., 2025).

Representative EMPA of phlogopite and amphibole (wt_ %)_

PhlogopiteAmphibole
SiO238.9339.6239.3239.4839.1638.9139.5338.844.7545.5844.20
TiO23.563.613.583.613.673.693.563.561.811.641.65
Al2O314.0313.9313.714.0114.0414.0713.7314.1111.4910.5211.25
FeO6.055.966.126.026.235.926.116.086.436.196.39
MnO0.020.04b.d.l0.040.020.030.020.060.130.090.1
MgO20.5921.2720.7520.9720.620.4720.8320.4616.5317.3516.96
CaOb.d.lb.d.l0.010.01b.d.l0.010.02b.d.l11.7811.711.85
Na2O0.570.560.550.570.580.590.570.571.811.751.79
K2O9.619.579.679.559.519.429.569.491.711.571.64
F2.953.042.953.142.793.002.652.87n.a1.50n.a
Cln.an.an.an.an.an.an.an.a0.020.020.02
BaO0.370.390.360.390.380.430.330.36n.an.an.a
Total96.679897.0397.896.9996.5496.9296.3696.4597.9195.85
Si(a.p.f.u)5.695.715.735.715.705.695.745.696.516.616.48
Ti0.390.390.390.390.400.410.390.390.200.180.18
Al2.422.372.352.392.412.432.352.441.981.801.94
AlVI 0.480.410.42
AlIV 1.491.391.52
Fe2+0.740.720.750.730.760.720.740.740.780.750.78
Mn 0.020.010.01
Mg4.494.574.514.524.474.474.514.473.593.753.71
Ca 1.840.821.86
Na0.160.160.160.160.160.170.160.160.510.490.51
Na (M4) 0.110.080.04
Na (A) 0.410.410.47
K1.791.761.801.761.771.761.771.770.320.290.31
F1.361.391.361.441.291.391.211.33
Mg#0.860.860.860.860.860.860.860.860.820.830.83
Na + K1.951.921.961.921.931.931.931.930.830.780.83

Representative EMPA of rutile and iron oxide (wt_%)

RutileIron oxide
SiO20.090.070.04
TiO296.7398.97b.d.l
Al2O30.180.05b.d.l
Cr2O30.94b.d,l0.02
Nb2O50.150.28b.d.l
FeO0.740.6590.50
MnOb.d.l.b.d.l0.03
CaO0.580.020.01
NiO0.03b.d.l0.14
ZnO0.010.020.03
V2O30.210.02b.d.l
Total99.65100.0990.78
Si (a.p.f.u)0.0010.001
Ti0.9800.993
Al0.0030.001
Cr0.010b.d.l
Nb0.0010.002
Fe2+0.0080.007
Ca0.008b.d.l.

Representative EMPA of pyroxene (wt_%)_

cpx

SiO252.5351.3451.0151.7352.4251.5851.4451.4151.552.16
TiO20.350.480.500.400.370.470.40.490.560.46
Al2O33.074.054.213.543.223.953.664.164.53.98
Cr2O30.310.380.40.380.320.400.380.400.390.40
FeO5.635.385.375.465.475.535.565.495.535.53
MnO0.160.110.170.160.170.130.160.150.140.12
MgO15.4714.9714.8515.2815.4214.9515.0414.8514.6814.95
CaO22.0022.0821.9621.9521.8221.9121.9921.9721.821.94
Na2O0.450.490.480.480.450.50.440.510.530.48
NiO0.010.010.02b.d.l0.040.020.010.010.020.01
Total99.9899.2898.9899.3999.7199.4499.0899.4499.64100.04
Si (a.p.f.u)1.931.91.891.911.931.91.911.91.91.91
Ti0.010.010.010.010.010.010.010.010.020.01
Al0.130.180.180.150.140.170.160.180.200.17
Cr0.010.010.010.010.010.010.010.010.010.01
Fe3+0.010.030.030.03 0.020.030.02
Fe2+0.160.140.140.140.160.150.140.150.170.17
Mn 0.01 0.01 0.01
Mg0.850.820.820.840.850.820.830.820.810.82
Ca0.870.870.870.870.860.870.870.870.860.86
Na0.030.040.030.030.030.040.030.040.040.03
Mg#0.840.860.860.860.840.840.850.850.830.83
AlVI0.060.070.080.060.070.080.070.080.090.09
AlIV0.070.100.110.090.070.100.090.100.100.09
AlVI/AlIV0.830.70.690.670.970.790.690.770.911.02
Wo45.9146.8846.9146.2445.946.5946.5346.8446.8446.63
En44.9244.244.1444.7945.1344.2344.2844.0343.8844.2
Fs9.178.928.958.988.989.189.199.149.289.17

opx

SiO253.8953.354.0254.2654.2754.5554.1653.7753.8453.7254.0754.2354.1254.1
TiO20.120.120.100.120.110.120.120.110.100.110.120.120.140.11
Al2O32.232.72.322.242.292.052.322.282.282.542.212.482.782.23
Cr2O30.170.230.170.140.170.130.200.200.210.230.200.230.250.15
FeO14.0714.2314.214.0814.2314.1714.1714.1914.0814.2414.1414.2514.2914.43
MnO0.30.280.280.290.280.270.290.290.310.280.290.270.310.29
MgO27.7927.6427.6527.4327.3927.7927.5427.3627.5527.4527.6127.3827.327.4
CaO0.890.610.780.750.750.830.800.850.860.700.810.800.730.78
Na2O0.030.010.030.020.020.010.020.030.020.090.02b.d.l0.030.02
NiO0.020.020.020.010.05b.d.l0.02b.d.l0.04b.d.l0.020.010.040.01
Total99.5199.1499.5999.3699.699.9199.6699.0799.399.3899.4899.7710099.53
Si (a.p.f.u)1.941.921.941.961.961.961.951.951.941.941.951.951.941.95
Al0.090.110.100.100.100.090.100.100.100.110.090.100.120.09
Fe3+0.020.020.01 0.010.01
Fe2+0.400.410.420.420.430.420.430.430.420.420.430.430.430.44
Mn0.010.010.010.010.010.010.010.010.010.010.010.010.010.01
Mg1.491.491.481.481.471.491.481.481.481.481.481.471.461.47
Ca0.030.020.030.030.030.030.030.030.030.030.030.030.030.03
Mg#0.790.790.780.780.770.780.780.780.780.780.780.770.770.77
AlVI0.030.040.040.050.050.040.050.040.040.040.040.060.060.05
AlIV0.060.080.060.040.040.040.050.060.060.060.050.050.060.05
AlVI/AlIV0.540.520.741.261.20.950.90.760.70.690.791.101.030.9
Wo1.761.211.551.511.511.651.581.691.711.41.621.61.461.56
En76.5176.6576.4276.4776.2776.4776.3776.1576.3976.3876.4276.1676.1775.98
Fs21.7422.1322.0322.0322.2221.8822.0522.1521.922.2221.9622.2422.3722.45

Major (wt_%) and trace elements (ppm) bulk rock compositions of the phlogopite-amphibole-plagioclase-bearing websterite xenolith of Guinadji volcano_

SiO2 (wt%)51.54
TiO20.43
Al2O34.88
Cr2O30.25
FeO*9.5
MnO0.19
MgO19.55
CaO12.98
Na2O0.58
K2O0.12
P2O50.07
BaO0.01
LOI0.32
Mg#0.79
Total100.42
Ba (ppm)100
Ce11.1
Cr1690
Cs0.05
Dy1.89
Er1.15
Eu0.61
Ga7.8
Gd2.07
Hf0.85
Ho0.41
La3.8
Lu0.12
Nb1.3
Nd8.4
Pr1.68
Rb3.9
Sc46.3
Sm2.36
Sr76.5
Tb0.35
Th0.2
Ti0.28
Tm0.12
U0.08
V248
Y9.3
Yb0.87
Zr30

Representative EMPA of plagioclase (wt_%)_

SiO252.9252.15
TiO2b.d.l0.01
Al2O329.0629.77
FeO0.140.15
MnO0.020.01
MgO0.050.06
CaO12.0412.60
Na2O4.424.04
K2O0.510.49
Total99.1799.28
Si (a.p.f.u)2.422.38
Al1.561.60
Fe2+0.010.01
Ca0.590.62
Na0.390.36
K0.030.03
An58.3061.47
Ab38.7535.71
Or2.942.82
DOI: https://doi.org/10.2478/mipo-2025-0011 | Journal eISSN: 1899-8526 | Journal ISSN: 1899-8291
Language: English
Page range: 103 - 119
Submitted on: Aug 10, 2025
|
Accepted on: Nov 18, 2025
|
Published on: Dec 31, 2025
In partnership with: Paradigm Publishing Services
Publication frequency: 1 issue per year

© 2025 Paterne Mulimbi Kagarabi, Theodoros Ntaflos, Jules Tamen, David G. Nkouathio, Kaniki Tumba, published by Mineralogical Society of Poland
This work is licensed under the Creative Commons Attribution 4.0 License.