Four-dimensional context of Earth's supercontinents

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Geochemical and mineralogical evidence that Rodinian assembly was unique Turmoil before the boring billion: Paleomagnetism of the 1880–1860 Ma Uatumã event in the Amazonian craton

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Four-dimensional context of Earth's supercontinents

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2016 nî lūn-bûn

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2016年の論文

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2016年学术文章

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2016年学术文章

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2016年学术文章

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2016年學術文章

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Four-dimensional context of Earth's supercontinents

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Four-dimensional context of Earth's supercontinents

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Four-dimensional context of Earth's supercontinents

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Four-dimensional context of Earth's supercontinents

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Four-dimensional context of Earth's supercontinents

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Four-dimensional context of Earth's supercontinents

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P1476

Four-dimensional context of Earth's supercontinents

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P2093

D. A. D. Evans

http://www.w3.org/2001/XMLSchema#string

J. B. Murphy

http://www.w3.org/2001/XMLSchema#string

Z. X. Li

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P2860

A plate tectonic model for the Paleozoic and Mesozoic constrained by dynamic plate boundaries and restored synthetic oceanic isochrons

The Phanerozoic record of global sea-level change

Origin of the Rheic Ocean: Rifting along a Neoproterozoic suture?

Proterozoic low orbital obliquity and axial-dipolar geomagnetic field from evaporite palaeolatitudes.

Absolute plate motions and true polar wander in the absence of hotspot tracks.

A positive test of East Antarctica-Laurentia juxtaposition within the Rodinia supercontinent.

Did the breakout of laurentia turn gondwanaland inside-out?

Supercontinent cycles and the calculation of absolute palaeolongitude in deep time.

Using seismic waves to image Earth's internal structure.

Assembly, configuration, and break-up history of Rodinia: A synthesis

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1-14

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scholarly article

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10.1144/SP424.12

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424

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2016-01-01T00:00:00Z

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2016GSLSP.424....1E

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supercontinent

Four-dimensional context of Earth's supercontinents

about

P2860

P2860

Four-dimensional context of Earth's supercontinents

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P1476

P2093

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