Xiao, Yilin

[["dc.bibliographiccitation.firstpage","5337"],["dc.bibliographiccitation.issue","17"],["dc.bibliographiccitation.journal","PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA"],["dc.bibliographiccitation.lastpage","5341"],["dc.bibliographiccitation.volume","112"],["dc.contributor.author","Herwartz, Daniel"],["dc.contributor.author","Pack, Andreas"],["dc.contributor.author","Krylov, Dmitri"],["dc.contributor.author","Xiao, Yilin"],["dc.contributor.author","Muehlenbachs, Karlis"],["dc.contributor.author","Sengupta, Sukanya"],["dc.contributor.author","Di Rocco, Tommaso"],["dc.date.accessioned","2018-11-07T09:58:18Z"],["dc.date.available","2018-11-07T09:58:18Z"],["dc.date.issued","2015"],["dc.description.abstract","The oxygen isotopic composition of hydrothermally altered rocks partly originates from the interacting fluid. We use the triple oxygen isotope composition (O-17/O-16, O-18/O-16) of Proterozoic rocks to reconstruct the O-18/O-16 ratio of ancient meteoric waters. Some of these waters have originated from snowball Earth glaciers and thus give insight into the climate and hydrology of these critical intervals in Earth history. For a Paleoproterozoic [similar to 2.3-2.4 gigayears ago (Ga)] snowball Earth, delta O-18 = -43 +/- 3 parts per thousand is estimated for pristine meteoric waters that precipitated at low paleo-latitudes (<= 35 degrees N). Today, such low O-18/O-16 values are only observed in central Antarctica, where long distillation trajectories in combination with low condensation temperatures promote extreme O-18 depletion. For a Neoproterozoic (similar to 0.6-0.7 Ga) snowball Earth, higher meltwater delta O-18 estimates of -21 +/- 3% imply less extreme climate conditions at similar paleolatitudes (<= 35 degrees N). Both estimates are single snapshots of ancient water samples and may not represent peak snowball Earth conditions. We demonstrate how O-17/O-16 measurements provide information beyond traditional O-18/O-16 measurements, even though all fractionation processes are purely mass dependent."],["dc.identifier.doi","10.1073/pnas.1422887112"],["dc.identifier.isi","000353554000040"],["dc.identifier.pmid","25870269"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/37341"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","0027-8424"],["dc.title","Revealing the climate of snowball Earth from Delta O-17 systematics of hydrothermal rocks"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","203"],["dc.bibliographiccitation.issue","1-2"],["dc.bibliographiccitation.journal","Earth and Planetary Science Letters"],["dc.bibliographiccitation.lastpage","213"],["dc.bibliographiccitation.volume","273"],["dc.contributor.author","Schmidt, Alexander"],["dc.contributor.author","Weyer, Stefan"],["dc.contributor.author","Mezger, Klaus"],["dc.contributor.author","Scherer, Erik E."],["dc.contributor.author","Xiao, Yilin"],["dc.contributor.author","Hoefs, Jochen"],["dc.contributor.author","Brey, Gerhard P."],["dc.date.accessioned","2018-11-07T11:11:59Z"],["dc.date.available","2018-11-07T11:11:59Z"],["dc.date.issued","2008"],["dc.description.abstract","The Qinling-Dabie-Sulu orogenic belt in eastern China is one of the largest ultrahigh-pressure (UHP) terranes worldwide. Mineral Sm-Nd- and zircon U-Pb dating has been widely used to reveal the metamorphic history of this collisional orogen. However, the exact timing of the UHP metamorphic event(s) remains controversial and ages ranging from 245 Ma to 220 Ma have been suggested. We present high precision garnet-cpx Lu-Hf ages for six eclogites from the Dabie and Sulu areas. All ages fall in a narrow range between 219.6 and 224.4 Ma. Five samples define a mean age of 223.0 +/- 0.9 Ma and one sample yields a slightly younger age of 219.6 +/- 1.4 Ma. This very tight age range is particularly remarkable considering the large regional distribution of sample localities (on the order of 100 km at the time of UHP metamorphism) and the wide variety of garnet and eclogite chemical compositions represented. Two samples yield Sm-Nd ages that are indistinguishable from their Lu-Hf ages, albeit with larger uncertainties. The identical ages of eclogites from both the Dabie and the Sulu region emphasize their close genetic relationship and similar metamorphic histories. The Lu-Hf results appear to date a punctuated event of garnet growth. Alternatively, the Lu-Hf garnet ages may represent the onset of rapid, contemporaneous uplift and subsequent cooling. However, trace element zoning of Lu and Hf is still preserved in garnet porphyroblasts, even in those with a homogeneous major element distribution. Thus, complete reequilibration of the Lu-Hf system during peak-temperature conditions probably did not occur. The garnet forming event can be placed toward the final stage of the UHP metamorphism, in agreement with some published U-Pb zircon ages. A possible trigger for this short-lived and widespread mineral growth episode may have been a fluid that became available at that stage of the metamorphic history. Although HREE-depleted patterns of older zircon grains may indicate the presence of an older generation of garnet, complete eclogitisation may have been inhibited during the major part of the prograde P-T path due to dry conditions during most of the UHP metamorphism. The uniform Lu-Hf (and Sm-Nd) ages of all investigated Dabie and Sulu eclogites suggest that garnet growth and thus possibly fluid availability were limited to a short time interval over a remarkably large regional scale. (C) 2008 Elsevier B.V. All rights reserved."],["dc.description.sponsorship","Deutsche Forschungsgemeinschaft (DFG) [WE 2850-2/1]"],["dc.identifier.doi","10.1016/j.epsl.2008.06.036"],["dc.identifier.isi","000259729000020"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/11244"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/53559"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Elsevier Science Bv"],["dc.relation.issn","1385-013X"],["dc.relation.issn","0012-821X"],["dc.relation.orgunit","Fakultät für Geowissenschaften und Geographie"],["dc.rights","CC BY-NC-ND 3.0"],["dc.rights.uri","http://creativecommons.org/licenses/by-nc-nd/3.0/"],["dc.title","Rapid eclogitisation of the Dabie-Sulu UHP terrane: Constraints from Lu-Hf garnet geochronology"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.artnumber","014512"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","PHYSICAL REVIEW B"],["dc.bibliographiccitation.volume","89"],["dc.contributor.author","Nandi, S."],["dc.contributor.author","Jin, W. T."],["dc.contributor.author","Xiao, Yilin"],["dc.contributor.author","Su, Y."],["dc.contributor.author","Price, Stephen D."],["dc.contributor.author","Shukla, D. K."],["dc.contributor.author","Strempfer, J."],["dc.contributor.author","Jeevan, Hirale S."],["dc.contributor.author","Gegenwart, Philipp"],["dc.contributor.author","Brueckel, T. H."],["dc.date.accessioned","2018-11-07T09:45:02Z"],["dc.date.available","2018-11-07T09:45:02Z"],["dc.date.issued","2014"],["dc.description.abstract","The magnetic structure of the Eu2+ moments in the superconducting EuFe2(As1-xPx)(2) sample with x = 0.15 has been determined using element-specific x-ray resonant magnetic scattering. Combining magnetic, thermodynamic, and scattering measurements, we conclude that the long-range ferromagnetic order of the Eu2+ moments aligned primarily along the c axis coexists with the bulk superconductivity at zero field. At an applied magnetic field >= 0.6 T, superconductivity still coexists with the ferromagnetic Eu2+ moments, which are polarized along the field direction. We propose a spontaneous vortex state for the coexistence of superconductivity and ;ferromagnetism in EuFe2(As0.85P0.15)(2)."],["dc.description.sponsorship","German Science Foundation [SPP 1458]"],["dc.identifier.doi","10.1103/PhysRevB.89.014512"],["dc.identifier.isi","000332230500003"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/34528"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Amer Physical Soc"],["dc.relation.issn","2469-9969"],["dc.relation.issn","2469-9950"],["dc.title","Coexistence of superconductivity and ferromagnetism in P-doped EuFe2As2"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","2018"],["dc.bibliographiccitation.issue","18"],["dc.bibliographiccitation.journal","Chinese Science Bulletin"],["dc.bibliographiccitation.lastpage","2023"],["dc.bibliographiccitation.volume","48"],["dc.contributor.author","Shen, K."],["dc.contributor.author","Zhang, Z. M."],["dc.contributor.author","van den Kerkhof, Alfons M."],["dc.contributor.author","Xiao, Y. L."],["dc.contributor.author","Xu, Z. Q."],["dc.contributor.author","Hoefs, Jochen"],["dc.date.accessioned","2018-11-07T10:36:23Z"],["dc.date.available","2018-11-07T10:36:23Z"],["dc.date.issued","2003"],["dc.description.abstract","Primary high-density fluid inclusions were identified in garnet from ultrahigh pressure eclogite in the southern part of the Sulu terrane. They occur isolatedly or in cluster together with relatively low-density two-phase inclusions. The eutectic temperature of the inclusions is as low as less than or equal to-52degreesC. A bubble was nucleated in a liquid inclusion during the specific stage of cyclic cooling-heating runs, and the liquid-gas homogenization temperature was measured to be less than or equal to-12.5degreesC. The composition of the inclusions modeled by the system CaCl2-NaCl-H2O, yields the fluid density of 1.27 g/cm(3) that corresponds to a pressure of ca. 2.4 GPa at the temperature of peak eclogite-facies metamorphism, close to the ultrahigh pressure metamorphic conditions. During the exhumation of the eclogite the inclusions reacted with the host mineral, forming hydrous silicate minerals that resulted in lowering of the fluid density and its transformation to multi-phase inclusions."],["dc.identifier.doi","10.1360/02wd0536"],["dc.identifier.isi","000185748100023"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/45311"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Science China Press"],["dc.relation.issn","1001-6538"],["dc.title","Unusual high-density and saline aqueous inclusions in ultrahigh pressure metamorphic rocks from Sulu terrane in eastern China"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.artnumber","1026"],["dc.bibliographiccitation.issue","6"],["dc.bibliographiccitation.journal","Contributions to Mineralogy and Petrology"],["dc.bibliographiccitation.volume","167"],["dc.contributor.author","Liu, Lei"],["dc.contributor.author","Xiao, Yilin"],["dc.contributor.author","Aulbach, Sonja"],["dc.contributor.author","Li, Dongyong"],["dc.contributor.author","Hou, Zhenhui"],["dc.date.accessioned","2018-11-07T09:39:14Z"],["dc.date.available","2018-11-07T09:39:14Z"],["dc.date.issued","2014"],["dc.description.abstract","Vanadium occurs in multiple valence states in nature, whereas Nb is exclusively pentavalent. Both are compatible in rutile, but the relationship of V-Nb partitioning and dependence on oxygen fugacity (expressed as fO(2)) has not yet been systematically investigated. We acquired trace-element concentrations on rutile grains (n = 86) in nine eclogitic samples from the Dabie-Sulu orogenic belt by laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) and combined them with published results in order to assess the direct and indirect effects of oxygen fugacity on the partitioning of V and Nb into rutile. A well-defined negative correlation between Nb (7-1,200 ppm) and V concentrations (50-3,200 ppm) was found, documenting a competitive relationship in the rutile crystal that does not appear to be controlled by bulk rock or mineral compositions. Based on the published relationship of D-Rt(V) and V valence with Delta QFM, we suggest that the priority order of V incorporation into rutile is V4+ > V3+ > V5+. The inferred Nb-V competitive relationship in rutile from the Dabie-Sulu orogenic belt could be explained by decreasing fO(2) due to dehydration reactions involving loss of oxidizing fluids during continental subduction: The increased proportion of V3+ (expressedas V3+/Sigma V) and attendant decrease in D-Rt(V) is suggested to lead to an increase in rutile lattice sites available for Nb5+. A similar effect may be observed under more oxidizing conditions. When V5+/Sigma V increases, D-Rt(V) shows a dramatic decline and Nb concentration increases considerably. This is possibly documented by rutile in highly metasomatized and oxidized MARID-type (MARID: mica-amphibole-rutile-ilmenite-diopside) mantle xenoliths from the Kaapvaal craton, which also show a negative V-Nb covariation. In addition, their Nb/Ta covaries with V concentrations: For V concentrations < 1,250 ppm, Nb/Ta ranges between 35 and 45, whereas for V > 1,250 ppm, Nb/Ta is considerably lower (5-15). This relationship is mainly controlled by a change in Nb concentrations, suggesting that the indirect dependence of D-Rt(Nb) on fO(2), which is not mirrored in D-Rt(Ta), can exert considerable influence on rutile Nb-Ta fractionation."],["dc.description.sponsorship","Natural Science Foundation of China [41172067, 41090372, 41273037]"],["dc.identifier.doi","10.1007/s00410-014-1026-2"],["dc.identifier.isi","000338344100001"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/33233"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Springer"],["dc.relation.issn","1432-0967"],["dc.relation.issn","0010-7999"],["dc.title","Vanadium and niobium behavior in rutile as a function of oxygen fugacity: evidence from natural samples"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","297"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","International Geology Review"],["dc.bibliographiccitation.lastpage","309"],["dc.bibliographiccitation.volume","47"],["dc.contributor.author","Zhang, Z. M."],["dc.contributor.author","Shen, K."],["dc.contributor.author","Xiao, Y. L."],["dc.contributor.author","van den Kerkhof, Alfons M."],["dc.contributor.author","Hoefs, Jochen"],["dc.contributor.author","Liou, J. G."],["dc.date.accessioned","2018-11-07T11:19:57Z"],["dc.date.available","2018-11-07T11:19:57Z"],["dc.date.issued","2005"],["dc.description.abstract","Rocks from the first pre-pilot hole of the Chinese Continental Scientific Drilling Project (CCSD-PPH1, 432 in), located in the eastern part of the Dabie-Sulu ultrahigh-pressure (UHP) metamorphic belt, have been subjected to a coesite-eclogite-facies metamorphic event, followed by an amphibolite-facies overprint. Primary fluid inclusions occur in garnet, omphacite, and apatite from eclogite; in kyanite and in topaz from quartzite; and in garnet, epidote, and apatite from paragneiss. Secondary fluid inclusions are present in all lithologies. Fluid inclusions are absent from ultramafic rocks. Based on fluid compositions and textural criteria we distinguished: (1) low-salinity aqueous-carbonic inclusions in topaz from quartzite, which may have originated from a supracrustal protolith; (2) primary CaCl2-NaCl-rich brine inclusions in garnet and in omphacite from eclogite and in kyanite from quartzite, representing UHP metamorphic fluids; (3) high-salinity aqueous-carbonic inclusions in quartz from eclogite and quartzite, representing amphibolite-facies fluids; (4) aqueous fluids of low- and intermediate salinity trapped as primary inclusions in garnet, epidote (or allanite) and apatite from gneiss, or as secondary inclusions, representing amphibolite-facies and later retrograde fluids; (5) carbonic inclusions are distributed along transgranular fractures in quartz from quartzite, and probably represent the latest retrograde fluid. The diversity in fluid inclusion populations and compositions from different vertical depths suggests a closed fluid system without large-scale fluid migration during UHP metamorphism. However, the common low- and medium-salinity inclusions in most rock types suggests that a water-dominated fluid from an external source infiltrated into the rock system during amphibolite-facies metamorphism, resulting in extensive retrogression of the UHP rocks."],["dc.identifier.doi","10.2747/0020-6814.47.3.297"],["dc.identifier.isi","000227403000005"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/55414"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","V H Winston & Son Inc"],["dc.relation.issn","0020-6814"],["dc.title","Fluid composition and evolution attending UHP metamorphism: Study of fluid inclusions from drill cores, southern Sulu Belt, Eastern China"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","292"],["dc.bibliographiccitation.journal","Journal of Asian Earth Sciences"],["dc.bibliographiccitation.lastpage","307"],["dc.bibliographiccitation.volume","172"],["dc.contributor.author","Liu, Haiyang"],["dc.contributor.author","Xiao, Yilin"],["dc.contributor.author","van den Kerkhof, Alfons"],["dc.contributor.author","Wang, Yangyang"],["dc.contributor.author","Zeng, Lingsen"],["dc.contributor.author","Guo, Haihao"],["dc.date.accessioned","2020-12-10T14:25:26Z"],["dc.date.available","2020-12-10T14:25:26Z"],["dc.date.issued","2019"],["dc.identifier.doi","10.1016/j.jseaes.2018.09.013"],["dc.identifier.issn","1367-9120"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/72553"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Metamorphism and fluid evolution of the Sumdo eclogite, Tibet: Constraints from mineral chemistry, fluid inclusions and oxygen isotopes"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1103"],["dc.bibliographiccitation.issue","9-10"],["dc.bibliographiccitation.journal","International Geology Review"],["dc.bibliographiccitation.lastpage","1129"],["dc.bibliographiccitation.volume","57"],["dc.contributor.author","Huang, Jian"],["dc.contributor.author","Xiao, Yilin"],["dc.date.accessioned","2018-11-07T09:54:29Z"],["dc.date.available","2018-11-07T09:54:29Z"],["dc.date.issued","2015"],["dc.description.abstract","Geochemical analyses of minerals and whole rocks for major and trace elements as well as Sr-Nd-O isotopes on samples along a profile across the boundary between amphibolite retrogressed from ultrahigh pressure (UHP) eclogite and its country rock granitic gneiss from the South Dabie low-T/UHP zone, China, are studied to assess the process that controls element mobility under extreme metamorphic conditions. Directly at the contact with the granitic gneiss, the amphibolite has higher concentrations of K, Al, LILEs, REEs, HFSEs, Th, and U, slightly lower concentrations of SiO2, MgO, and CaO, but very similar FeOt and transitional metal element contents relative to the other amphibolites further away from the boundary. Consistently, delta O-18 values of the amphibolite display a progressive increase towards the boundary, indicating fluid-assisted O-isotope exchange across the contacts of different lithologies at local scales. These can neither be attributed to amphibolite-facies retrogression of eclogite, which is known to have no significant effect on their major and trace elements, nor to Si-rich metasomatism from partially melted granitic gneiss, which should increase the silica content of the amphibolite at the contact. Therefore, neither of the two processes is viable here. We thus propose that the variations observed here were caused by metasomatism of supercritical liquids that were generated at pressure higher than that of the second critical endpoint in the granitic gneiss-H2O system. This interpretation is supported by multiphase solid inclusions of K-feldspar+quartz+ calcite+zircon +/- amphibole +/- clinozoisite +/- garnet +/- apatite within garnet in the amphibolite."],["dc.identifier.doi","10.1080/00206814.2014.893213"],["dc.identifier.isi","000354780600002"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/36544"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Taylor & Francis Inc"],["dc.relation.issn","1938-2839"],["dc.relation.issn","0020-6814"],["dc.title","Element mobility in mafic and felsic ultrahigh-pressure metamorphic rocks from the Dabie UHP Orogen, China: insights into supercritical liquids in continental subduction zones"],["dc.type","review"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1160"],["dc.bibliographiccitation.issue","11"],["dc.bibliographiccitation.journal","International Geology Review"],["dc.bibliographiccitation.lastpage","1177"],["dc.bibliographiccitation.volume","47"],["dc.contributor.author","Zhang, Z. M."],["dc.contributor.author","Xiao, Y. L."],["dc.contributor.author","Hoefs, Jochen"],["dc.contributor.author","Xu, Z. Q."],["dc.contributor.author","Liou, J. G."],["dc.date.accessioned","2018-11-07T10:54:40Z"],["dc.date.available","2018-11-07T10:54:40Z"],["dc.date.issued","2005"],["dc.description.abstract","The Pre-pilot Hole No. 1 of the Chinese Continental Scientific Drilling Project (CCSD-PPH1) in the southern Sulu terrane recovered a continuous core of eclogite, garnet peridotite, orthogneiss, paragneiss, and minor schist and quartzite. Geochemical characteristics indicate that the garnet peridotite was derived from depleted mantle; all other rock types are metamorphosed supracrustal rocks with continental affinities. The eclogite consists of garnet, omphacite, phengite, quartz (coesite), amphibole, rutile, and zircon; P-T estimates of peak metamorphism are 785-820 degrees C and >2.7 to 3.7 GPa. The gneisses show common amphibolite-facies mineral assemblages consisting of plagioclase, K-feldspar, muscovite, and quartz, with minor garnet, epidote (or zoisite), and biotite; coesite inclusions in zircon indicate that the gneisses together with eclogites were subjected to an early UHP metamorphism prior to amphibolite-facies retrogression. The Garnet peridotites show porphyroblastic textures, and consist mainly of garnet, clinopyroxene, orthopyroxene, and olivine with minor phlogopite. Garnet and clinopyroxene porphyroblasis show significant compositional zoning. Applying relevant geothermobarometers, core compositions of the minerals indicate P-T conditions of 6.0-7.0 GPa and 1100-1200 degrees C. For the rim, similar or slightly higher P-T conditions compared to the eclogites were obtained. We suggest that the former represent crystallization conditions of garnet peridotite in the upper mantle, whereas the latter reflect reequilibrium conditions during incorporation of mantle rocks into the subducted slab. We conclude that the garnet peridotite may have been derived from the mantle wedge above the subduction zone. If so, these mantle-derived rocks were sandwiched between continental-derived country rocks."],["dc.identifier.doi","10.2747/0020-6814.47.11.1160"],["dc.identifier.isi","000232750200005"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/49618"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","V H Winston & Son Inc"],["dc.relation.issn","0020-6814"],["dc.title","Petrogenesis of UHP metamorphic crustal and Mande rocks from the Chinese Continental Scientific Drilling Pre-pilot Hole 1, Sulu belt, eastern China"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.artnumber","094407"],["dc.bibliographiccitation.issue","9"],["dc.bibliographiccitation.journal","PHYSICAL REVIEW B"],["dc.bibliographiccitation.volume","90"],["dc.contributor.author","Nandi, S."],["dc.contributor.author","Jin, W. T."],["dc.contributor.author","Xiao, Yilin"],["dc.contributor.author","Su, Y."],["dc.contributor.author","Price, Stephen D."],["dc.contributor.author","Schmidt, W."],["dc.contributor.author","Schmalzl, K."],["dc.contributor.author","Chatterji, T."],["dc.contributor.author","Jeevan, Hirale S."],["dc.contributor.author","Gegenwart, Philipp"],["dc.contributor.author","Brueckel, Th."],["dc.date.accessioned","2018-11-07T09:35:21Z"],["dc.date.available","2018-11-07T09:35:21Z"],["dc.date.issued","2014"],["dc.description.abstract","The magnetic structure of the Eu2+ moments in the superconducting EuFe2(As1-xPx)(2) sample with x = 0.19 has been determined using neutron scattering. We conclude that the Eu2+ moments are aligned along the c direction below T-C = 19.0(1) K with an ordered moment of 6.6(2) mu(B) in the superconducting state. An impurity phase similar to the underdoped phase exists within the bulk sample which orders antiferromagnetically below T-N = 17.0(2) K. We found no indication of iron magnetic order, nor any incommensurate magnetic order of the Eu2+ moments in the sample."],["dc.description.sponsorship","German Science Foundation [SPP 1458]"],["dc.identifier.doi","10.1103/PhysRevB.90.094407"],["dc.identifier.isi","000342432100002"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/32363"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Amer Physical Soc"],["dc.relation.issn","1550-235X"],["dc.relation.issn","1098-0121"],["dc.title","Magnetic structure of the Eu2+ moments in superconducting EuFe2(As1-xPx)(2) with x=0.19"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]