<?xml version="1.0" encoding="UTF-8"?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-10-30T03:26:34Z</responseDate><request verb="GetRecord" identifier="oai:munzur-rdlopen.rawdatalibrary.net:munzur/975" metadataPrefix="oai_dc">https://munzur-rdlopen.rawdatalibrary.net/oai/request</request><GetRecord><record><header><identifier>oai:munzur-rdlopen.rawdatalibrary.net:munzur/975</identifier><datestamp>2026-10-28T15:28:22Z</datestamp><setSpec>openaire</setSpec><setSpec>com_munzur_1</setSpec><setSpec>col_munzur_2</setSpec><setSpec>com_munzur_12</setSpec><setSpec>col_munzur_165</setSpec></header><metadata><oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd"><dc:title>Identification and source provenance of jadeite-bearing jade axes from Ulucak Höyük, Western Anatolia</dc:title><dc:creator>Sayit, Kaan</dc:creator><dc:creator>Çevik, Özlem</dc:creator><dc:creator>Aktağ, Alican</dc:creator><dc:creator>Erdoğu, Burçin</dc:creator><dc:creator>Bamyacı, Onur</dc:creator><dc:creator>Vuruşkan, Osman</dc:creator><dc:creator>Sivil, Coşkun</dc:creator><dc:subject>geochemistry</dc:subject><dc:subject>ICP-MS</dc:subject><dc:subject>jade</dc:subject><dc:subject>petrography</dc:subject><dc:subject>Ulucak Höyük</dc:subject><dc:description>The jades from Ulucak Höyük (İzmir, Turkey) are green-colored in hand specimen, and combined petrographic, XRD, and whole-rock analyses indicate that they mainly comprise jadeitic clinopyroxene, characterizing them as jadeite-bearing jades. Primitive mantle (PM)-normalized multi-element patterns reveal two distinct chemical groups. Both groups display depletion in Th and U; however, Group 1 shows a narrower elemental range and marked positive Pb anomaly. The second group, on the other hand, displays a wide elemental range in most elements and strong negative anomalies in Zr and Hf ([Nd/Zr]PM = 1.6–4.2; [Sm/Hf]PM = 1.8–3.5). Regarding REE systematics, both groups are characterized by weak positive slopes ([La/Yb]Ch = 1.7–5.3). However, whereas Group 1 shows coherent LREE-enriched trends, Group 2 displays flat- to LREE-enriched patterns with a wide range in Eu. When the geochemical features of Ulucak jades are compared with the high-pressure (HP) metamorphic rocks from Turkey and Greece, the similar multi-element patterns of Syros eclogites (Greece) to Group 2 Ulucak jades make Syros a possible source area for the Ulucak artefacts. On the other hand, the geochemical resemblance of the Sifnos jadeite-bearing gneisses to Group 1 Ulucak jades may raise the possibility of this island being another source for the Ulucak jades.</dc:description><dc:publisher>John Wiley and Sons Inc</dc:publisher><dc:date>2025</dc:date><dc:type>Article</dc:type><dc:identifier>https://rdlopen.rawdatalibrary.net/r/munzur/975</dc:identifier><dc:identifier>https://doi.org/10.1111/arcm.13102</dc:identifier><dc:identifier>0003-813X</dc:identifier><dc:language>en</dc:language><dc:relation>Archaeometry</dc:relation><dc:rights>info:eu-repo/semantics/closedAccess</dc:rights><dc:type>info:eu-repo/semantics/article</dc:type><dc:identifier>https://munzur-rdlopen.rawdatalibrary.net/tr/items/munzur/975</dc:identifier></oai_dc:dc></metadata></record></GetRecord></OAI-PMH>