The Fuchuan Ophiolite in South China: Evidence for modern‐style plate tectonics during Rodinia breakup

نویسندگان

چکیده

Subduction initiation processes, such as those evidenced in the Izu-Bonin-Mariana (IBM) forearc crust are a key feature of modern-style plate tectonics. However, evidence for this process Precambrian is limited, due to scarcity ophiolite suites and particular lack typical complete ophiolitic sequences similar observed Phanerozoic ophiolites. Mineral analyses olivine, orthopyroxene, chrome spinel from harzburgite two types clinopyroxene cumulate gabbro Fuchuan ophiolite, South China suggest formation Neoproterozoic subduction system IBM. High temperature (1,000–1,200°C), low pressure along with high degree melt extraction (>18%) have been recorded harzburgite. This evidence, conjunction magma evolution basalt boninite hydrous calc-alkaline magmatism, crustal section indicates transition initial mature setting. Statistical analysis global ophiolites through time suggests that IBM-like systems may successfully operated since at least latest (ca. 1,000 Ma) be pervasive on Earth ca. 850 Ma. Additional India, Siberia, Arabian-Nubian Shield, which also IBM cold deep became much more common around periphery Rodinia supercontinent. acted geodynamic trigger break-up Rodinia.

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ژورنال

عنوان ژورنال: Geochemistry Geophysics Geosystems

سال: 2021

ISSN: ['1525-2027']

DOI: https://doi.org/10.1029/2021gc010137