South-verging early folds: An important element in the structure of the northern Green Mountains
- Cornell Coll., Mt. Vernon, IA (United States). Geology Dept.
Reconnaissance mapping in the Camels Hump Group, Mt. Mansfield 7.5[prime] quadrangle, north-central Vermont, indicates more complex structures than those portrayed on previously published maps. Preliminary interpretation for the structure around Smugglers Notch, for example, is that an early recumbent syncline with Hazens Notch Formation in its center (including the Sterling Pond talc deposits), opens to the south. The early syncline is deformed by the north-northeast trending Green Mountain anticlinorium, which at Smugglers Notch plunges gently south. Thus the mass of Underhill Formation along the summit ridge of Mt. Mansfield is on the upper, overturned limb of the early fold, and on the west limb of the open, upright anticlinorium. The lowest cliffs in Smugglers Notch are Underhill Formation on the upright limb of the early fold. Rocks of the intervening, intensely weathered and graphitic Hazens Notch Formation are especially prone to the rock slides for which Smugglers Notch is infamous. Early minor isoclinal folds and strongly developed quartz rods and lineations trend roughly east-west. Correlation of this fabric with east-west lineations and poorly preserved fold hinges in the Camels Hump area farther south will help correlate deformational sequences between the two areas. Early minor folds that are roughly coaxial with younger Green Mountain folds are much less common in the Mt. Mansfield area than to the south, and faulting seems to have been much less intense. Thus following marker horizons such as quartzite beds and greenstones around fold hinges may be more successful. Do south-directed structures indicate lateral movement of material toward the Vermont reentrant during the Taconian orogeny
- OSTI ID:
- 5505504
- Report Number(s):
- CONF-9303211-; CODEN: GAAPBC
- Journal Information:
- Geological Society of America, Abstracts with Programs; (United States), Vol. 25:2; Conference: 28. annual Geological Society of America (GSA) Northeastern Section meeting, Burlington, VT (United States), 22-24 Mar 1993; ISSN 0016-7592
- Country of Publication:
- United States
- Language:
- English
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