Geochemical characteristics and 40Ar- 39Ar ages of the amphibolites and gabbros in Tarlang area: Implications for tectonic evolution of the Chinese Altai

Abstract

Amphibolitic and gabbroic rocks occur in Tarlang area in Chinese Altay. Amphibolites are metamorphosed products of mafic magmatic rocks (SiO 2 = 45.42% - 52.96%) and contain high Al 2O 3 (13.14% - 17.92%), Fe 2O 3 T (9.08% - 16.88%) and TiO 2 (0.82% - 3.23%) contents. The amphibolite samples show relatively flat REE patterns, without significant fractionations of REEs (La/Yb N = 1.53 - 1.79). These samples are depleted in HFSEs slightly, with slightly Ti-Nb-Ta negative anomalies, which suggest a subtle relation to subduction-related environment. The gabbroic samples (SiO 2 = 46.96% - 49.86%) have intermediate TiO 2 (0.38% - 1.89%) and relatively low K 2 O contents (K 2 O = 0.34% - 1.03%), belonging to subalkali rocks (Na 2 O > K 2 O). They have relatively high Al 2O 3 (15.0% - 20.81%), CaO (10.13% - 11.60%) and moderate MgO (7.3% - 8.3% ) contents. The gabbroic samples show two types of REE patterns. One is characterized by slight fractionation of REEs (La/Yb N = 1.10 - 1.67) and weak Eu anomalies (δEu = 1.03 - 1.10), while the other is enriched in LREE s (La/Yb N = 5.97 - 6.39), with significantly positive Eu anomalies (δEu = 1.31 - 1.44), which may reflect accumulation of plagioclase in the magma chamber. These gabbroic rocks all exhibit Ti-Nb-Ta troughs and Pb-Sr spikes, also implying a subduction-related origin. The 40Ar/ 39Ar spectrum of the gabbroic sample is simple and flat (plateau age of 266.9 ± 4.2Ma; isochron age of 261 ± 23Ma), indicating that its K-Ar isotopic system was not seriously disturbed by subsequent thermal events and may reflect the intrusion time of the gabbro. However, 40Ar- 39Ar analysis of the amphibolite give rise to a saddle-like spectrum, and its youngest plateau (297.3 ± 6.1Ma) probably reflects the last metamorphic event. The difference on age and geochemistry between the amphibolitic and gabbroic rocks implies that they probably represent different mafic magma. The protolith of amphibolites probably formed in a seamount near a subduction zone and subsequently accreated to the Altai. The gabbro exhibits subduction-releted characteristics and was coeval with transtensional movement in the Chinese Altai, probably reflecting a tectonic transition in the Permian.

阿爾泰塔爾浪地區出露一些斜長角閃巖和輝長巖。其中,斜長角閃巖為基性巖漿巖變質的產物,SiO_2含量為45.42%～52.96%,具有較高的Al_2O_3(13.14%～17.92%)、Fe_2O_3~T(9.08%～16.88%)和TiO_2(0.82%～3.23%)含量。斜長角閃巖樣品稀土元素曲線比較平坦,輕重稀土元素分餾不明顯(La/Yb_N=1.53～1.79),無明顯的Nb和Ta虧損。通過野外產狀及地球化學特征分析,認為該斜長角閃巖形成于海山的構造環境。輝長巖SiO_2(46.96%～49.86%)含量稍低,TiO_2(0.38%～1.89%)變化較大,并富Al_2O_3(15.0%～20.81%)、CaO(10.13%～11.60%),具有中等至較高MgO含量(7.3%～8.3%)和相對較低的鉀含量(K_2O=0.34%～1.03%),屬亞堿性巖石系列(Na_2O>K_2O)。輝長巖呈現兩種稀土元素組成特征。一種輕重稀土分餾不明顯,配分曲線比較平坦(La/Yb_N=1.10～1.67),具有輕微的Eu正異常(δEu=1.03～1.10);另一種輕重稀土元素分餾較明顯(La/Yb_N=5.97～...