Arc-generated metavolcanic rocks in the Anshan–Benxi greenstone belt, North China Craton: Constraints from geochemistry and zircon U–Pb–Hf isotopic systematics

Abstract

The Anshan–Benxi granite-greenstone belt (ABGB) in the Eastern Block of the North China Craton mainly comprises supracrustal rocks of amphibole plagioclase gneisses, plagioclase amphibolites, chlorite schists, biotite schists, quartzites and banded iron formations (BIFs), and intrusive monzogranitic to syenogranitic gneisses. Based on geology, spatial distributions, lithologies and zircon U-Pb geochronology, the metavolcanic rocks of the southern ABGB can be divided into the ∼2527Ma southern plagioclase gneiss group, ∼2536Ma southern amphibolite group, ∼2574 to 2560Ma northern chlorite schist group and northern amphibolite group from south to north. These rocks outcrop as stratified and stratoid beds, whereas some occur as enclaves within later intrusive K-rich granitic gneisses. The southern plagioclase gneiss group exhibits calc-alkaline andesite compositions with high MgO, Cr, and Ni, fractionated REE patterns and depletion in Nb–Ta, which resemble high magnesian andesite (HMA) and are derived from the partial melting of sub-arc mantle peridotite that was previously metasomatized by slab melts. The southern amphibolite group has tholeiitic basalt compositions with slight enrichment in LREEs and high Nb–Ti concentrations but low (Nb/La)PM ratios, which coincide with Nb-enriched basalt and are generated by the remelting of residues of sub-arc mantle after the extraction of HMA melts. The northern schist group shows high-K calc-alkaline andesite-dacite compositions and have highest silica and potassium, and obvious enrichment in LREEs and LILEs and depletion in Nb–Ta, which are comparable to the sanukitoid series rocks. These rocks probably formed by low-degree partial melting of a sub-arc mantle wedge that was metasomatized by slab-derived fluids. The northern amphibolite group exhibits tholeiite compositions with unfractionated REE patterns and low (Nb/La)PM ratios, which are consistent with back-arc basin basalts (BABB) and are produced by partial melting of depleted mantle.Combined with lithological associations of the HMA, NEB, sanukitoid-like rocks and BABB-like rocks, the Anshan–Benxi granite-greenstone belt was produced under a convergent plate environment. Both the zircon εHf values and petrogenesis indicate that the four groups of the metamorphic volcanic rocks directly contributed to continental crustal growth. Integrating with the widespread ∼2.5Ga syenogranites and subordinate K-rich granitoids that were derived from reworking of ancient crust, we propose that the ABGB experienced a significant episode of continental growth dominated by a subduction-related lateral accretion accompanied with contemporaneously strong reworking of ancient crustal materials.