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Shen-Su Sun

Researcher at University of Adelaide

Publications -  33
Citations -  36830

Shen-Su Sun is an academic researcher from University of Adelaide. The author has contributed to research in topics: Basalt & Mantle (geology). The author has an hindex of 28, co-authored 33 publications receiving 33103 citations. Previous affiliations of Shen-Su Sun include State University of New York System & Australian National University.

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The composition of the Earth

TL;DR: In this paper, the authors compared the relative abundances of the refractory elements in carbonaceous, ordinary, and enstatite chondritic meteorites and found that the most consistent composition of the Earth's core is derived from the seismic profile and its interpretation, compared with primitive meteorites, and chemical and petrological models of peridotite-basalt melting relationships.
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Lead isotopic study of young volcanic rocks from mid-ocean ridges, ocean islands and island arcs

TL;DR: Lead isotopic compositions of young volcanic rocks from different tectonic environments have distinctive characteristics their differences are evaluated within the framework of global tectonics and mantle differentiation Ocean island leads are in general more radiogenic than mid-ocean ridge basalt (morb) leads as discussed by the authors.
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Collision of the North China and Yangtse Blocks and formation of coesite-bearing eclogites: Timing and processes☆

TL;DR: In this article, the uplift history of eclogite in the Dabie Mountains can be subdivided into two stages: (1) fast uplift driven by thrust during continental-continental collision and deep subduction (at 221 Ma) of the continental crust; (2) later gentle uplift with rise of the Dabbie Mountains in the late Jurassic and Cretaceous (at 134 Ma).
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Geochemical characteristics of mid-ocean ridge basalts

TL;DR: In this article, a strong correlation exists between percent TiO 2 (proportional to amount of melting) and Al 2 O 3 /TiO 2, CaO/TiO2 ratios of these close to primary MORB, indicating a progressive release of Al and Ca from the mantle source.