Hadean geodynamics inferred from time-varying 142Nd/144Nd in the early Earth rock record
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Hadean geodynamics inferred from time-varying 142Nd/144Nd in the early Earth rock record. / Saji, N.s.; Larsen, K.; Wielandt, D.; Schiller, M.; Costa, M.m.; Whitehouse, M.j.; Rosing, M.t.; Bizzarro, M.
In: Geochemical Perspectives Letters, Vol. 7, 2018, p. 43-48.Research output: Contribution to journal › Journal article › Research › peer-review
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TY - JOUR
T1 - Hadean geodynamics inferred from time-varying 142Nd/144Nd in the early Earth rock record
AU - Saji, N.s.
AU - Larsen, K.
AU - Wielandt, D.
AU - Schiller, M.
AU - Costa, M.m.
AU - Whitehouse, M.j.
AU - Rosing, M.t.
AU - Bizzarro, M.
PY - 2018
Y1 - 2018
N2 - Tracking the secular evolution of 142Nd/144Nd anomalies is important towards understanding the crust-mantle dynamics in the early Earth. Excessive scatter in the published data, however, precludes identifying the fine structure of 142Nd/144Nd evolution as the expected variability is on the order of few parts per million. We report ultra-high precision 142Nd/144Nd data for Eoarchean and Palaeoarchean rocks from the Isua Supracrustal Belt (SW Greenland) that show a well-resolved 142Nd/144Nd temporal variability suggesting progressive convective homogenisation of the Hadean Isua depleted mantle. This temporally decreasing 142Nd/144Nd signal provides a direct measure of early mantle dynamics, defining a stirring timescale of <250 Myr consistent with vigorous convective stirring in the early mantle. The 142Nd/144Nd evolution suggests protracted crustal residence times of ~1000-2000 Myr, inconsistent with modern-style plate tectonics in the Archean. In contrast, a stagnant-lid regime punctuated by episodes of mantle overturns accounts for the long life-time estimated here for the Hadean proto-crust.
AB - Tracking the secular evolution of 142Nd/144Nd anomalies is important towards understanding the crust-mantle dynamics in the early Earth. Excessive scatter in the published data, however, precludes identifying the fine structure of 142Nd/144Nd evolution as the expected variability is on the order of few parts per million. We report ultra-high precision 142Nd/144Nd data for Eoarchean and Palaeoarchean rocks from the Isua Supracrustal Belt (SW Greenland) that show a well-resolved 142Nd/144Nd temporal variability suggesting progressive convective homogenisation of the Hadean Isua depleted mantle. This temporally decreasing 142Nd/144Nd signal provides a direct measure of early mantle dynamics, defining a stirring timescale of <250 Myr consistent with vigorous convective stirring in the early mantle. The 142Nd/144Nd evolution suggests protracted crustal residence times of ~1000-2000 Myr, inconsistent with modern-style plate tectonics in the Archean. In contrast, a stagnant-lid regime punctuated by episodes of mantle overturns accounts for the long life-time estimated here for the Hadean proto-crust.
U2 - 10.7185/geochemlet.1818
DO - 10.7185/geochemlet.1818
M3 - Journal article
VL - 7
SP - 43
EP - 48
JO - Geochemical Perspectives Letters
JF - Geochemical Perspectives Letters
SN - 2410-3403
ER -
ID: 212301417