Результаты исследований: Материалы конференций › тезисы › Рецензирование
Оценка количества взвеси материала гидротермального плюма в металлоносных осадках рудного узла Семенов (Срединно-Атлантический хребет). / Кукса, Катерина Александровна.
2024. 43-47 Реферат от Металлогения древних и современных океанов-2024. РУДОГЕНЕЗ, Российская Федерация.Результаты исследований: Материалы конференций › тезисы › Рецензирование
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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