Thermochronologic constraints on uplifting events since the early cretaceous in the north margin of the Luxi rise, eastern China

Guozhi Wang , Shugen Liu , Can Zou

Journal of Earth Science ›› 2013, Vol. 24 ›› Issue (4) : 579 -588.

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Journal of Earth Science ›› 2013, Vol. 24 ›› Issue (4) : 579 -588. DOI: 10.1007/s12583-013-0351-0
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Thermochronologic constraints on uplifting events since the early cretaceous in the north margin of the Luxi rise, eastern China

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Abstract

Two 40Ar/39Ar ages and six fission track ages from monzonite and the Jurassic-Cretaceous rocks provide new geochronologic constraints on the timing of uplifting events in the north margin of the Luxi (鲁西) rise, eastern China. 40Ar/39Ar age 111.1±2.4 and 111.2±2.5 Ma of biotite and K-feldspar sampled from the monzonite may record the cooling age at 300 and 150–300 °C, respectively. Fission track ages of zircon and apatite from the monzonite changing from 75±7 to 40±3 Ma record the cooling age at 250 and 120 °C, respectively. The apatite from the Jurassic-Cretaceous sandstone and volcanic rocks yielded a different T-t path. The results indicate that there are two phases 111-46.9 and 13.4 (6.5)-0 Ma of rapid uplifting happened to the north margin of the Luxi rise; the first one is a tilted uplift from north to south in Zibo (淄博) during 111-46.9 Ma and in the south in Mengshan (蒙山) during 70-40 Ma; the second one is a tilted uplift from south to north in Mengshan during 32-20 Ma, and in turn in Taishan (泰山) and Zibo during 23-20 and 13.4-0 or 6.5-0 Ma, respectively. The aging coincidence between magmatism and tectonic uplifting implies there are two phases of uplifting induced by large scale extension and lithospheric thinning.

Keywords

Luxi rise / apatite fission track / T-t path / closure temperature / uplift

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Guozhi Wang, Shugen Liu, Can Zou. Thermochronologic constraints on uplifting events since the early cretaceous in the north margin of the Luxi rise, eastern China. Journal of Earth Science, 2013, 24(4): 579-588 DOI:10.1007/s12583-013-0351-0

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