TY - JOUR

T1 - Magmatic complexes of the Tekturmas Fold-and-Thrust Belt, Central Kazakhstan: An overview and new implications for the early Paleozoic evolution of the Paleo-Asian Ocean

AU - Safonova, Inna

AU - Gurova, Alexandra

AU - Perfilova, Alina

AU - Xiao, Wenjiao

AU - Kotler, Pavel

AU - Seltmann, Reimar

AU - Soloshenko, Natalia

AU - Dolgopolova, Alla

N1 - We appreciate mutual discussions about the Tekturmas Fold-and-Thrust Belt with RAS Academician K. Degtyarev and Dr. A. Yakubchuk. The study was supported by the Ministry of Science and Higher Education of Russia, State Assignment Projects (122041400044-2, FSUS-2025-0008; 123011800012-9), National Natural Science Foundation of China (W2431031), State Administration of Foreign Experts Affairs (Y20240079).

PY - 2025/6

Y1 - 2025/6

N2 - The Tekturmas Fold-and-Thrust Belt (TFTB) is an important structure of the Kazakhstan Orocline in the western Central Asian Orogenic Belt (CAOB), which formation is linked with the early-middle Paleozoic evolution of the Paleo-Asian Ocean (PAO). The TFTB includes accreted oceanic sediments and magmatic rocks, supra-subduction ophiolites and fore-arc and back-arc siliciclastic rocks of Cambrian to Silurian ages. There remains a deficiency in data from magmatic rocks of the TFTB and, as a result, the timing of magmatism, mantle sources and tectonic settings are still debatable and the general early Paleozoic evolution of the TFTB is not fully understood. In this paper we review previous geological and age data (U-Pb, microfauna) and present new geological, geochronological (U-Pb zircon ages) and geochemical data and first isotope data (Sm-Nd, Pb-Pb, Lu-Hf). We discuss these new results and the previously reported, but still limited data from both magmatic and clastic rocks. Granite and rhyolite yielded middle-late Ordovician U-Pb zircon ages, 462 and 449 Ma, respectively. There are three main groups of volcanic/subvolcanic and plutonic rocks: (1) high-Ti, (2) mid-Ti, and (3) low-Ti. The high-Ti basalts and andesites are enriched in high-field strength elements (HFSE) and light rare-earth elements (LREE); they were derived at 2–4 % melting of an enriched garnet-bearing peridotite (εNdt = +2.1… +6.8; 206Pb/204Pb = 19.2–22.8) and erupted on an oceanic island or seamount. The mid-Ti gabbro is N-MORB formed from a 15 % melted depleted mantle source (εNdt = +8.1; 206Pb/204Pb = 18.9). The low-Ti group is depleted in HFSE, but not LREE, and formed at high degrees of melting (15–30 %) of depleted and ultra-depleted mantle sources (εNdt = +6.1… +10.8; εHft = +17.6… +19.3) suggesting their emplacement in a supra-subduction setting. Based on all the available data, we present a model of double-sided subduction in this part of the PAO, which generated four intra-oceanic arcs at its opposite sides: early-middle Cambrian and Early Ordovician on one side and Early and Late Ordovician on another side. The early-middle Cambrian and Early Ordovician arcs were tectonically eroded and their fragments have been preserved in blocks of mélange and greywacke sandstones only. The pieces of all arcs were tectonically juxtaposed in the TFTB during the processes of subduction and accretion in the PAO. The early Paleozoic magmatism ceased in early Silurian time.

AB - The Tekturmas Fold-and-Thrust Belt (TFTB) is an important structure of the Kazakhstan Orocline in the western Central Asian Orogenic Belt (CAOB), which formation is linked with the early-middle Paleozoic evolution of the Paleo-Asian Ocean (PAO). The TFTB includes accreted oceanic sediments and magmatic rocks, supra-subduction ophiolites and fore-arc and back-arc siliciclastic rocks of Cambrian to Silurian ages. There remains a deficiency in data from magmatic rocks of the TFTB and, as a result, the timing of magmatism, mantle sources and tectonic settings are still debatable and the general early Paleozoic evolution of the TFTB is not fully understood. In this paper we review previous geological and age data (U-Pb, microfauna) and present new geological, geochronological (U-Pb zircon ages) and geochemical data and first isotope data (Sm-Nd, Pb-Pb, Lu-Hf). We discuss these new results and the previously reported, but still limited data from both magmatic and clastic rocks. Granite and rhyolite yielded middle-late Ordovician U-Pb zircon ages, 462 and 449 Ma, respectively. There are three main groups of volcanic/subvolcanic and plutonic rocks: (1) high-Ti, (2) mid-Ti, and (3) low-Ti. The high-Ti basalts and andesites are enriched in high-field strength elements (HFSE) and light rare-earth elements (LREE); they were derived at 2–4 % melting of an enriched garnet-bearing peridotite (εNdt = +2.1… +6.8; 206Pb/204Pb = 19.2–22.8) and erupted on an oceanic island or seamount. The mid-Ti gabbro is N-MORB formed from a 15 % melted depleted mantle source (εNdt = +8.1; 206Pb/204Pb = 18.9). The low-Ti group is depleted in HFSE, but not LREE, and formed at high degrees of melting (15–30 %) of depleted and ultra-depleted mantle sources (εNdt = +6.1… +10.8; εHft = +17.6… +19.3) suggesting their emplacement in a supra-subduction setting. Based on all the available data, we present a model of double-sided subduction in this part of the PAO, which generated four intra-oceanic arcs at its opposite sides: early-middle Cambrian and Early Ordovician on one side and Early and Late Ordovician on another side. The early-middle Cambrian and Early Ordovician arcs were tectonically eroded and their fragments have been preserved in blocks of mélange and greywacke sandstones only. The pieces of all arcs were tectonically juxtaposed in the TFTB during the processes of subduction and accretion in the PAO. The early Paleozoic magmatism ceased in early Silurian time.

KW - Central Asian Orogenic Belt

KW - Intra-oceanic arcs

KW - Isotopes

KW - Paleo-Asian Ocean

KW - Seamounts

KW - U-Pb zircon ages

UR - https://www.mendeley.com/catalogue/35e8a42a-6b86-3fe9-a304-7ea6cc5d82b2/

UR - https://www.scopus.com/record/display.uri?eid=2-s2.0-105001692429&origin=inward&txGid=35638163817d00722fdefe2d2177efc7

U2 - 10.1016/j.earscirev.2025.105120

DO - 10.1016/j.earscirev.2025.105120

M3 - Article

VL - 265

JO - Earth-Science Reviews

JF - Earth-Science Reviews

SN - 0012-8252

M1 - 105120

ER -