Tectonostratigraphy of the Lesser Himalaya of Bhutan: Implications for the along-strike stratigraphic continuity of the northern Indian margin

被引:106
作者
Long, Sean [1 ]
McQuarrie, Nadine [1 ]
Tobgay, Tobgay [1 ]
Rose, Catherine [1 ]
Gehrels, George [2 ]
Grujic, Djordje [3 ]
机构
[1] Princeton Univ, Dept Geosci, Princeton, NJ 08544 USA
[2] Univ Arizona, Dept Geosci, Tucson, AZ 85721 USA
[3] Dalhousie Univ, Dept Earth Sci, Halifax, NS B3H 4J1, Canada
基金
美国国家科学基金会;
关键词
FOLD-THRUST BELT; MAIN CENTRAL THRUST; TECTONIC EVOLUTION; STRUCTURAL EVOLUTION; CONTINENTAL-MARGIN; ZIRCON AGES; INVERTED METAMORPHISM; GREENSCHIST FACIES; SHUMAR ALLOCHTHON; EASTERN HIMALAYA;
D O I
10.1130/B30202.1
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
New mapping in eastern Bhutan, in conjunction with U-Pb detrital zircon and delta C-13 data, defines Lesser Himalayan tectonostratigraphy. The Daling-Shumar Group, 2-6 km of quartzite (Shumar Formation) overlain by 3 km of schist (Daling Formation), contains similar to 1.8-1.9 Ga intrusive orthogneiss bodies and youngest detrital zircon peaks, indicating a Paleoproterozoic deposition age. The Jaishidanda Formation, 0.5-1.7 km of garnet-biotite schist and quartzite, stratigraphically overlies the Daling Formation beneath the Main Central thrust, and yields youngest detrital zircon peaks ranging from similar to 0.8-1.0 Ga to ca. 475 Ma, indicating a Neoproterozoic-Ordovician(?) deposition age range. The Baxa Group, 2-3 km of quartzite, phyllite, and dolomite, overlies the Daling-Shumar Group in the foreland, and yields ca. 0.9 Ga to ca. 520 Ma youngest detrital zircon peaks, indicating a Neoproterozoic-Cambrian(?) deposition age range. Baxa dolo mite overlying quartzite containing ca. 525 Ma detrital zircons yielded delta C-13 values between +3% and +6%, suggesting deposition during an Early Cambrian positive delta C-13 excursion. Above the Baxa Group, the 2-3 km thick Diuri Formation diamictite yielded a ca. 390 Ma youngest detrital zircon peak, suggesting correlation with the late Paleozoic Gondwana supercontinent glaciation. Finally, the Permian Gondwana succession consists of sandstone, siltstone, shale, and coal. Our deposition age data from Bhutan: (1) reinforce suggestions that Paleoproterozoic (similar to 1.8-1.9 Ga) Lesser Himalayan deposition was continuous along the entire northern Indian margin; (2) show a likely east ward continuation of a Permian over Cambrian unconformity in the Lesser Himalayan section identified in Nepal and northwest India; and (3) indicate temporal overlap between Neoproterozoic-Paleozoic Lesser Himalayan (proximal) and Greater Himalayan-Tethyan Himalayan (distal) deposition.
引用
收藏
页码:1406 / 1426
页数:21
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