Thermal consequences of mantled gneiss dome emplacement
- 1 July 1989
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 93 (3-4) , 392-404
- https://doi.org/10.1016/0012-821x(89)90038-1
Abstract
No abstract availableKeywords
This publication has 15 references indexed in Scilit:
- Some thermal and mechanical consequences of rapid uplift: an example from the Southern Alps, New ZealandEarth and Planetary Science Letters, 1987
- Creation and preservation of subduction‐related inverted metamorphic gradientsJournal of Geophysical Research, 1987
- Controls on the Apparent Thermal and Baric Structure of Mountain BeltsThe Journal of Geology, 1987
- Two-dimensional modeling of the P-T-t paths of regional metamorphism in simple overthrust terrainsGeology, 1987
- The Acadian Thermal History of the Merrimack Synclinorium in New HampshireThe Journal of Geology, 1985
- Heat focussing, granite genesis and inverted metamorphic gradients in continental collision zonesEarth and Planetary Science Letters, 1985
- New radiometric ages on gneisses of the Oliverian domes in New Hampshire and MassachusettsAmerican Journal of Science, 1985
- Pressure--Temperature--Time Paths of Regional Metamorphism I. Heat Transfer during the Evolution of Regions of Thickened Continental CrustJournal of Petrology, 1984
- Age and Origin of the Oliverian Domes, Central-Western New HampshireGSA Bulletin, 1969
- Geology of the Mascoma quadrangle, New HampshireGSA Bulletin, 1939