Ultramafic–mafic and granitoids supra‐subduction magmatism in the southern Ashanti volcanic belt, Ghana: Evidence from geochemistry and Nd isotopes

Samuel B. Dampare; Tsugio Shibata; Daniel K. Asiedu; Osamu Okano; Shiloh K.D. Osae; David Atta‐Peters; Patrick A. Sakyi

doi:10.1002/gj.3512

Ultramafic–mafic and granitoids supra‐subduction magmatism in the southern Ashanti volcanic belt, Ghana: Evidence from geochemistry and Nd isotopes

Geological Journal ◽

10.1002/gj.3512 ◽

2020 ◽

Vol 55 (4) ◽

pp. 2495-2531 ◽

Cited By ~ 2

Author(s):

Samuel B. Dampare ◽

Tsugio Shibata ◽

Daniel K. Asiedu ◽

Osamu Okano ◽

Shiloh K.D. Osae ◽

...

Keyword(s):

Volcanic Belt ◽

Nd Isotopes ◽

Subduction Magmatism

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Temporal control of subduction magmatism in the eastern Trans-Mexican Volcanic Belt: Mantle sources, slab contributions, and crustal contamination

Geochemistry Geophysics Geosystems ◽

10.1029/2003gc000524 ◽

2003 ◽

Vol 4 (8) ◽

Cited By ~ 69

Author(s):

Arturo Gómez-Tuena ◽

Alexandra B. LaGatta ◽

Charles H. Langmuir ◽

Steven L. Goldstein ◽

Fernando Ortega-Gutiérrez ◽

...

Keyword(s):

Crustal Contamination ◽

Volcanic Belt ◽

Temporal Control ◽

Mexican Volcanic Belt ◽

Mantle Sources ◽

Trans Mexican Volcanic Belt ◽

Subduction Magmatism

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Decision letter for "Petrogenesis and ore potential of Permian mafic intrusions in the Dacaotan area, eastern Tianshan: Constraints from whole‐rock platinum‐group element contents and Sr–Nd isotopes"

10.1002/gj.3999/v2/decision1 ◽

2020 ◽

Keyword(s):

Platinum Group Element ◽

Group Element ◽

Nd Isotopes ◽

Eastern Tianshan ◽

Mafic Intrusions ◽

Element Contents ◽

Platinum Group ◽

Ore Potential

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The Chingandzha flora of the Okhotsk-Chukotka volcanic belt

Palaeobotany ◽

10.31111/palaeobotany/2019.10.13 ◽

2019 ◽

Vol 10 ◽

pp. 13-179

Author(s):

L. B. Golovneva

Keyword(s):

River Basin ◽

Volcanic Belt ◽

Flowering Plants ◽

Sedimentary Deposits ◽

North East ◽

The North ◽

Magadan Region ◽

Chukotka Volcanic Belt ◽

Systematic Composition ◽

Coastal Lowlands

The Chingandzha flora comes from the volcanic-sedimentary deposits of the Chingandzha Formation (the Okhotsk-Chukotka volcanic belt, North-East of Russia). The main localities of the Chingandzha flora are situated in the Omsukchan district of the Magadan Region: on the Tap River (basin of the middle course of the Viliga River), on the Kananyga River, near the mouth of the Rond Creek, and in the middle reaches of the Chingandzha River (basin of the Tumany River). The Chingandzha flora includes 23 genera and 33 species. Two new species (Taxodium viligense Golovn. and Cupressinocladus shelikhovii Golovn.) are described, and two new combinations (Arctopteris ochotica (Samyl.) Golovn. and Dalembia kryshtofovichii (Samyl.) Golovn.) are created. The Chingandzha flora consists of liverworts, horsetails, ferns, seed ferns, ginkgoaleans, conifers, and angiosperms. The main genera are Arctop teris, Osmunda, Coniopteris, Cladophlebis, Ginkgo, Sagenoptepis, Sequoia, Taxodium, Metasequoia, Cupressinocladus, Protophyllocladus, Pseudoprotophyllum, Trochodendroides, Dalembia, Menispermites, Araliaephyllum, Quereuxia. The Chingandzha flora is distinct from other floras of the Okhotsk-Chukotka volcanic belt (OCVB) in predominance of flowering plants and in absence of the Early Cretaceous relicts such as Podozamites, Phoenicopsis and cycadophytes. According to its systematic composition and palaeoecological features, the Chingandzha flora is similar to the Coniacian Kaivayam and Tylpegyrgynay floras of the North-East of Russia, which were distributed at coastal lowlands east of the mountain ridges of the OCVB. Therefore, the age of the Chingandzha flora is determined as the Coniacian. This flora is assigned to the Kaivayam phase of the flora evolution and to the Anadyr Province of the Siberian-Canadian floristic realm. The Chingandzha flora is correlated with the Coniacian Aleeky flora from the Viliga-Tumany interfluve area and with other Coniacian floras of the OCVB: the Chaun flora of the Central Chukotka, the Kholchan flora of the Magadan Region and the Ul’ya flora of the Ul’ya Depression.

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