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Оценка количества взвеси материала гидротермального плюма в металлоносных осадках рудного узла Семенов (Срединно-Атлантический хребет). / Кукса, Катерина Александровна.

2024. 43-47 Abstract from Металлогения древних и современных океанов-2024. РУДОГЕНЕЗ, Russian Federation.

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@conference{ed5b51fd943a4d8486415da3a7746e6d,
title = "Оценка количества взвеси материала гидротермального плюма в металлоносных осадках рудного узла Семенов (Срединно-Атлантический хребет)",
abstract = "Mineralogical and geochemical features of three cores of proximal metalliferous sediments from the Semenov hydrothermal sulfide cluster were studied in order to decipher the evolution of fluid discharge. Iron has a dual origin in core sediments: from hydrothermal plume fallout and mass-wasted sulfide deposits. A novel approach of quantitatively assess the relative amount of plume fallout matter allowed us to reconstruct the temporal variations of hydrothermal activity within the Semenov-1, 2 and 4 fields, which lasted permanently for about ~43 kyr with varying intensity.",
author = "Кукса, {Катерина Александровна}",
year = "2024",
language = "русский",
pages = "43--47",
note = "Металлогения древних и современных океанов-2024. РУДОГЕНЕЗ ; Conference date: 22-04-2024 Through 25-04-2024",

}

RIS

TY - CONF

T1 - Оценка количества взвеси материала гидротермального плюма в металлоносных осадках рудного узла Семенов (Срединно-Атлантический хребет)

AU - Кукса, Катерина Александровна

PY - 2024

Y1 - 2024

N2 - Mineralogical and geochemical features of three cores of proximal metalliferous sediments from the Semenov hydrothermal sulfide cluster were studied in order to decipher the evolution of fluid discharge. Iron has a dual origin in core sediments: from hydrothermal plume fallout and mass-wasted sulfide deposits. A novel approach of quantitatively assess the relative amount of plume fallout matter allowed us to reconstruct the temporal variations of hydrothermal activity within the Semenov-1, 2 and 4 fields, which lasted permanently for about ~43 kyr with varying intensity.

AB - Mineralogical and geochemical features of three cores of proximal metalliferous sediments from the Semenov hydrothermal sulfide cluster were studied in order to decipher the evolution of fluid discharge. Iron has a dual origin in core sediments: from hydrothermal plume fallout and mass-wasted sulfide deposits. A novel approach of quantitatively assess the relative amount of plume fallout matter allowed us to reconstruct the temporal variations of hydrothermal activity within the Semenov-1, 2 and 4 fields, which lasted permanently for about ~43 kyr with varying intensity.

M3 - тезисы

SP - 43

EP - 47

T2 - Металлогения древних и современных океанов-2024. РУДОГЕНЕЗ

Y2 - 22 April 2024 through 25 April 2024

ER -

ID: 119316247