Eynatten, Hilmar von

[["dc.bibliographiccitation.firstpage","36"],["dc.bibliographiccitation.journal","Sedimentary Geology"],["dc.bibliographiccitation.lastpage","52"],["dc.bibliographiccitation.volume","306"],["dc.contributor.author","Krippner, Anne"],["dc.contributor.author","Meinhold, Guido"],["dc.contributor.author","Morton, Andrew C."],["dc.contributor.author","von Eynatten, Hilmar"],["dc.date.accessioned","2018-11-07T09:39:39Z"],["dc.date.available","2018-11-07T09:39:39Z"],["dc.date.issued","2014"],["dc.description.abstract","This work is an attempt to evaluate six different garnet discrimination diagrams (one binary diagram and five ternary diagrams) commonly used by many researchers. The mineral chemistry of detrital garnet is a useful tool in sedimentary provenance studies, yet there is no clear-cut understanding of what garnet type originates from which host lithology. Several discrimination diagrams exist for garnet showing distinct compositional fields, separated by strict boundaries that are thought to reflect specific types of source rocks. For this study, a large dataset was compiled (N = 3532) encompassing major element compositions of garnets derived from various host lithologies, including metamorphic, igneous, and mantle-derived rocks, in order to test the applicability of the various discrimination schemes. The dataset contains mineral chemical data collected from the literature complemented with some new data (N = 530) from garnet-bearing metamorphic and ultramafic rocks in Austria and Norway. Discrimination of the tested diagrams only works for a small group of garnets derived from mantle rocks, granulite-facies metasedimentary rocks, and felsic igneous rocks. For other garnet types, the assignment to a certain type of host rock remains ambiguous. This is considered insufficient and therefore the evaluated diagrams should be used with great care. We further apply compositional biplot analysis to derive some hints towards future perspectives in detrital garnet discrimination. (c) 2014 Elsevier B.V. All rights reserved."],["dc.description.sponsorship","CASP; German Research Foundation (DFG) [EY 23/20-1]"],["dc.identifier.doi","10.1016/j.sedgeo.2014.03.004"],["dc.identifier.isi","000336707200003"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/33334"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Elsevier Science Bv"],["dc.relation.issn","1879-0968"],["dc.relation.issn","0037-0738"],["dc.title","Evaluation of garnet discrimination diagrams using geochemical data of garnets derived from various host rocks"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","121"],["dc.bibliographiccitation.journal","Sedimentary Geology"],["dc.bibliographiccitation.lastpage","126"],["dc.bibliographiccitation.volume","389"],["dc.contributor.author","Stalder, Roland"],["dc.contributor.author","von Eynatten, Hilmar"],["dc.contributor.author","Costamoling, Julian"],["dc.contributor.author","Potrafke, Alexander"],["dc.contributor.author","Dunkl, István"],["dc.contributor.author","Meinhold, Guido"],["dc.date.accessioned","2020-12-10T15:21:17Z"],["dc.date.available","2020-12-10T15:21:17Z"],["dc.date.issued","2019"],["dc.identifier.doi","10.1016/j.sedgeo.2019.06.001"],["dc.identifier.issn","0037-0738"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/16767"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/72975"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.notes.intern","Merged from goescholar"],["dc.rights","CC BY-NC-ND 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by-nc-nd/4.0"],["dc.title","OH in detrital quartz grains as tool for provenance analysis: Case studies on various settings from Cambrian to Recent"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","815"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","International Journal of Earth Sciences"],["dc.bibliographiccitation.lastpage","832"],["dc.bibliographiccitation.volume","104"],["dc.contributor.author","Caracciolo, Luca"],["dc.contributor.author","Critelli, Salvatore"],["dc.contributor.author","Cavazza, W."],["dc.contributor.author","Meinhold, Guido"],["dc.contributor.author","von Eynatten, Hilmar"],["dc.contributor.author","Manetti, Piero"],["dc.date.accessioned","2018-11-07T09:59:16Z"],["dc.date.available","2018-11-07T09:59:16Z"],["dc.date.issued","2015"],["dc.description.abstract","Detrital heavy mineral analysis coupled with a regional geological review provide key elements to re-evaluate the distribution of the Rhodope metamorphic zone (SE Europe) in the region and its role in determining the evolution of the Thrace basin. We focus on the Eocene-Oligocene sedimentary successions exposed in the southern Thrace basin margin to determine the dispersal pathways of eroded crustal elements, of both oceanic and continental origins, as well as their different contributions through time. Lithological aspects and tectonic data coupled with geochemistry and geochronology of metamorphic terranes exposed in the area point to a common origin of tectonic units exposed in NW Turkey (Biga Peninsula) with those of NE Greece and SE Bulgaria (Rhodope region). The entire region displays (1) common extensional signatures, consisting of comparable granitoid intrusion ages, and a NE-SW sense of shear (2) matching zircon age populations between the metapelitic and metamafic rocks of the Circum-Rhodope Belt (NE Greece) and those of the Camlica-Kemer complex and Cetmi m,lange exposed in NW Turkey. Detrital heavy mineral abundances from Eocene-Oligocene sandstones of the southern Thrace basin demonstrate the influence of two main sediment sources mostly of ultramafic/ophiolitic and low- to medium-grade metamorphic lithologies, plus a third, volcanic source limited to the late Eocene-Oligocene. Detrital Cr-spinel chemistry is used to understand the origin of the ultramafic material and to discriminate the numerous ultramafic sources exposed in the region. Compositional and stratigraphic data indicate a major influence of the metapelitic source in the eastern part (Gallipoli Peninsula) during the initial stages of sedimentation with increasing contributions from metamafic sources through time. On the other hand, the western and more external part of the southern Thrace margin (Gok double dagger eada, Samothraki and Limnos) displays compositional signatures according to a mixed provenance from the metapelitic and metamafic sources of the Circum-Rhodope Belt (CamlA +/- ca-Kemer complex and Cetmi m,lange). Tectonic restoration and compositional signatures provide constraints on the Palaeogene palaeogeography of this sector of the central-eastern Mediterranean region."],["dc.description.sponsorship","MIUR-PRIN Project [2009PBA7FL_001]"],["dc.identifier.doi","10.1007/s00531-014-1111-9"],["dc.identifier.isi","000351519400017"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/37554"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Springer"],["dc.relation.issn","1437-3262"],["dc.relation.issn","1437-3254"],["dc.title","The Rhodope Zone as a primary sediment source of the southern Thrace basin (NE Greece and NW Turkey): evidence from detrital heavy minerals and implications for central-eastern Mediterranean palaeogeography"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","387"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","International Journal of Earth Sciences"],["dc.bibliographiccitation.lastpage","388"],["dc.bibliographiccitation.volume","106"],["dc.contributor.author","Caracciolo, Luca"],["dc.contributor.author","Meinhold, Guido"],["dc.contributor.author","Critelli, Salvatore"],["dc.contributor.author","von Eynatten, Hilmar"],["dc.contributor.author","Manetti, Piero"],["dc.date.accessioned","2018-11-07T10:29:08Z"],["dc.date.available","2018-11-07T10:29:08Z"],["dc.date.issued","2017"],["dc.identifier.doi","10.1007/s00531-016-1302-7"],["dc.identifier.isi","000393646000022"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/43578"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","PUB_WoS_Import"],["dc.publisher","Springer"],["dc.relation.issn","1437-3262"],["dc.relation.issn","1437-3254"],["dc.title","Comment on Maravelis et al. \"Accretionary prism-forearc interactions as reflected in the sedimentary fill of southern Thrace Basin (Lemnos Island, NE Greece)\""],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dc.type.subtype","letter_note"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","320"],["dc.bibliographiccitation.journal","Gondwana Research"],["dc.bibliographiccitation.lastpage","329"],["dc.bibliographiccitation.volume","87"],["dc.contributor.author","Schönig, Jan"],["dc.contributor.author","von Eynatten, Hilmar"],["dc.contributor.author","Meinhold, Guido"],["dc.contributor.author","Lünsdorf, N. Keno"],["dc.contributor.author","Willner, Arne P."],["dc.contributor.author","Schulz, Bernhard"],["dc.date.accessioned","2021-04-14T08:32:02Z"],["dc.date.available","2021-04-14T08:32:02Z"],["dc.date.issued","2020"],["dc.identifier.doi","10.1016/j.gr.2020.06.020"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/83786"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-399"],["dc.relation.issn","1342-937X"],["dc.title","Deep subduction of felsic rocks hosting UHP lenses in the central Saxonian Erzgebirge: Implications for UHP terrane exhumation"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","320"],["dc.bibliographiccitation.journal","Gondwana Research"],["dc.bibliographiccitation.lastpage","323"],["dc.bibliographiccitation.volume","98"],["dc.contributor.author","Schönig, Jan"],["dc.contributor.author","von Eynatten, Hilmar"],["dc.contributor.author","Meinhold, Guido"],["dc.contributor.author","Lünsdorf, N. Keno"],["dc.contributor.author","Willner, Arne P."],["dc.contributor.author","Schulz, Bernhard"],["dc.date.accessioned","2021-09-01T06:42:33Z"],["dc.date.available","2021-09-01T06:42:33Z"],["dc.date.issued","2021"],["dc.identifier.doi","10.1016/j.gr.2020.12.029"],["dc.identifier.pii","S1342937X21000253"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/89083"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-455"],["dc.relation.issn","1342-937X"],["dc.title","Reply to comment on “Deep subduction of felsic rocks hosting UHP lenses in the central Saxonian Erzgebirge: Implications for UHP terrane exhumation”"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","32"],["dc.bibliographiccitation.journal","Sedimentary Geology"],["dc.bibliographiccitation.lastpage","49"],["dc.bibliographiccitation.volume","376"],["dc.contributor.author","Schönig, Jan"],["dc.contributor.author","Meinhold, Guido"],["dc.contributor.author","von Eynatten, Hilmar"],["dc.contributor.author","Lünsdorf, Nils K."],["dc.date.accessioned","2020-12-10T15:21:17Z"],["dc.date.available","2020-12-10T15:21:17Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.1016/j.sedgeo.2018.07.009"],["dc.identifier.issn","0037-0738"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/72974"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Provenance information recorded by mineral inclusions in detrital garnet"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","14"],["dc.bibliographiccitation.journal","Sedimentary Geology"],["dc.bibliographiccitation.lastpage","26"],["dc.bibliographiccitation.volume","375"],["dc.contributor.author","Tolosana-Delgado, Raimon"],["dc.contributor.author","von Eynatten, Hilmar"],["dc.contributor.author","Krippner, Anne"],["dc.contributor.author","Meinhold, Guido"],["dc.date.accessioned","2020-12-10T15:21:17Z"],["dc.date.available","2020-12-10T15:21:17Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.1016/j.sedgeo.2017.11.003"],["dc.identifier.issn","0037-0738"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/72972"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","A multivariate discrimination scheme of detrital garnet chemistry for use in sedimentary provenance analysis"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1421"],["dc.bibliographiccitation.issue","8"],["dc.bibliographiccitation.journal","Geological Magazine"],["dc.bibliographiccitation.lastpage","1440"],["dc.bibliographiccitation.volume","158"],["dc.contributor.author","Schönig, Jan"],["dc.contributor.author","von Eynatten, Hilmar"],["dc.contributor.author","Meinhold, Guido"],["dc.contributor.author","Lünsdorf, N. Keno"],["dc.date.accessioned","2021-08-12T07:44:48Z"],["dc.date.available","2021-08-12T07:44:48Z"],["dc.date.issued","2021"],["dc.description.abstract","Abstract Detrital coesite-bearing garnet is the final product of a complex geological cycle including coesite entrapment at ultra-high-pressure conditions, exhumation to Earth’s surface, erosion and sedimentary transport. In contrast to the usual enrichment of high-grade metamorphic garnet in medium- to coarse-sand fractions, coesite-bearing grains are often enriched in the very-fine-sand fraction. To understand this imbalance, we analyse the role of source-rock lithology, inclusion size, inclusion frequency and fluid infiltration on the grain-size heterogeneity of coesite-bearing garnet based on a dataset of 2100 inclusion-bearing grains, of which 93 contain coesite, from the Saxonian Erzgebirge, Germany. By combining inclusion assemblages and garnet chemistry, we show that (1) mafic garnet contains a low number of coesite inclusions per grain and is enriched in the coarse fraction, and (2) felsic garnet contains variable amounts of coesite inclusions per grain, whereby coesite-poor grains are enriched in the coarse fraction and coesite-rich grains extensively disintegrated into smaller fragments resulting in an enrichment in the fine fraction. Raman images reveal that: small coesite inclusions of dimension < 9 µm are primarily monomineralic, whereas larger inclusions partially transformed to quartz; and garnet fracturing, fluid infiltration and the coesite-to-quartz transformation is a late process during exhumation taking place at c.  330°C. A model for the disintegration of coesite-bearing garnet enables the heterogeneous grain-size distribution to be explained by inclusion frequency. High abundances of coesite inclusions cause a high degree of fracturing and fracture connections to smaller inclusions, allowing fluid infiltration and the transformation to quartz, which in turn further promotes garnet disintegration."],["dc.identifier.doi","10.1017/S0016756821000017"],["dc.identifier.pii","S0016756821000017"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/88298"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-448"],["dc.relation.eissn","1469-5081"],["dc.relation.issn","0016-7568"],["dc.relation.orgunit","Geowissenschaftliches Zentrum"],["dc.rights","CC BY 4.0"],["dc.title","Life-cycle analysis of coesite-bearing garnet"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","715"],["dc.bibliographiccitation.issue","8"],["dc.bibliographiccitation.journal","Geology"],["dc.bibliographiccitation.lastpage","718"],["dc.bibliographiccitation.volume","47"],["dc.contributor.author","Schönig, Jan"],["dc.contributor.author","von Eynatten, Hilmar"],["dc.contributor.author","Meinhold, Guido"],["dc.contributor.author","Lünsdorf, N. Keno"],["dc.date.accessioned","2020-12-10T18:37:08Z"],["dc.date.available","2020-12-10T18:37:08Z"],["dc.date.issued","2019"],["dc.identifier.doi","10.1130/G46253.1"],["dc.identifier.issn","0091-7613"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/76852"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Diamond and coesite inclusions in detrital garnet of the Saxonian Erzgebirge, Germany"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]