Reference health
Intensive hydration of the mantle transition zone beneath China caused by ancient slab stagnation
28/28 checkable references clean · checked 2026-07-14
Every reference with a DOI in the deposited reference list resolved to a known work in Crossref or DataCite at the dated check, and none carried a publisher retraction, withdrawal, or removal notice.
2 without a DOI — not checked. A reference deposited without a DOI is never matched by title or guessed at; it stays outside the checked set, and this line discloses that.
The 28 checked references that resolve
resolves10.1029/94GL02965
Hydrous modified spinel, Mg<sub>1.75</sub>SiH<sub>0.5</sub>O<sub>4</sub>: A new water reservoir in the mantle transition region
resolves10.1016/j.pepi.2003.09.015
Water transport into the deep mantle and formation of a hydrous transition zone
resolves10.1016/j.epsl.2010.11.038
Water distribution across the mantle transition zone and its implications for global material circulation
resolves10.1016/j.epsl.2009.02.027
A joint interpretation of electromagnetic and seismic tomography models suggests the mantle transition zone below Europe is dry
resolves10.1016/j.pepi.2008.11.009
Seismic image and origin of the Changbai intraplate volcano in East Asia: Role of big mantle wedge above the stagnant Pacific slab
resolves10.1016/j.rgg.2009.11.006
The role of water in the deep upper mantle and transition zone: dehydration of stagnant slabs and its effects on the big mantle wedge
resolves10.1016/j.lithos.2006.09.015
Geochemistry of Cenozoic basalts and mantle xenoliths in Northeast China
resolves10.1016/j.lithos.2009.02.007
Intraplate magmatism related to deceleration of upwelling asthenospheric mantle: Implications from the Changbaishan shield basalts, northeast China
resolves10.1016/0012-821X(91)90127-4
Major element, REE, and Pb, Nd and Sr isotopic geochemistry of Cenozoic volcanic rocks of eastern China: implications for their origin from suboceanic-type mantle reservoirs
resolves10.1093/petrology/43.6.981
Lamproites from Gaussberg, Antarctica: Possible Transition Zone Melts of Archaean Subducted Sediments
resolves10.1029/2002GC000421
Sr‐Nd‐Pb composition of Mesozoic Pacific oceanic crust (Site 1149 and 801, ODP Leg 185): Implications for alteration of ocean crust and the input into the Izu‐Bonin‐Mariana subduction system
resolves10.1016/j.chemgeo.2007.10.008
Mantle dynamics beneath East Asia constrained by Sr, Nd, Pb and Hf isotopic systematics of ultramafic xenoliths and their host basalts from Hannuoba, North China
resolves10.1016/j.epsl.2008.02.028
Subduction recycling of continental sediments and the origin of geochemically enriched reservoirs in the deep mantle
resolves10.1016/0012-821X(89)90079-4
The geochemistry of marine sediments, island arc magma genesis, and crust-mantle recycling
resolves10.1007/s00410-008-0303-3
Influence of temperature, composition, silica activity and oxygen fugacity on the H2O storage capacity of olivine at 8 GPa
resolves10.1016/S0040-1951(01)00132-9
Cenozoic episodic volcanism and continental rifting in northeast China and possible link to Japan Sea development as revealed from K–Ar geochronology
resolves10.1016/0012-821X(75)90088-6
Approximation of terrestrial lead isotope evolution by a two-stage model
The 2 references without a DOI — listed, not checked
no DOI — not checkedSmyth, J. R. β-Mg2SiO4: A potential host for water in the mantle? Am. Mineral. 72, 1051–1055 (1987).
no DOI — not checkedCousens, B. L. & Allan, J. F. A Pb, Sr, and Nd isotopic study of basaltic rocks from the Sea of Japan, LEGS 127/128. Proc. Ocean Drill. Program Sci. Results 127–128, 805–817 (1992).
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