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Data Publisher for Earth & Environmental Science

Kashintsev, Georgy L; Shreider, Anatoly A; Maksimochkin, V I; Bulychev, A A; Gilod, D A (2008): Composition of basalts from the Romanche Fracture Zone [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.746786, Supplement to: Kashintsev, GL et al. (2008): Transtension and alkaline magmatism of the Romanche Fracture Zone. Geotektonika, No 4, 85-92, https://doi.org/10.1134/S0016852108040055

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Abstract:
New magnetometric, petrological, and geochemical data on basalts from the central Romanche Fracture Zone allow to classify these rocks into two groups. Igneous rocks from the active part of the fracture zone that have undergone transtension are referred to alkaline rocks. According to some indications, they are younger that oceanic tholeiites of the southern fault-line ridge, which were affected by elevated pressure in the past. These data indicate with a high probability that the Romanche Fracture Zone belongs to a rare group of magmatically active demarcation transform lines that separate large oceanic domains different in structural and geochemical features.
Project(s):
Coverage:
Median Latitude: -0.828840 * Median Longitude: -21.230248 * South-bound Latitude: -1.086600 * West-bound Longitude: -21.688600 * North-bound Latitude: -0.644000 * East-bound Longitude: -20.909100
Event(s):
G96-29 * Latitude: -1.086600 * Longitude: -20.991500 * Location: Romanche fracture zone * Campaign: G96 * Basis: Gelendzhik
G96-34 * Latitude: -0.644000 * Longitude: -20.909100 * Location: Romanche fracture zone * Campaign: G96 * Basis: Gelendzhik
G96-42 * Latitude: -0.970000 * Longitude: -21.688600 * Location: Romanche fracture zone * Campaign: G96 * Basis: Gelendzhik
Size:
2 datasets

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