Synform
نویسندگان
چکیده
منابع مشابه
The rise of solid-state diapirs
When magma’inside a diapir solidifies it increases in density and becomes a stiff power-law fluid. If the diapir is still positively (or negatively) buoyant after solidification, it will continue to rise (or start to sink). The results presented here suggest that solidified diapirs may rise (sink) a distance of up to a few kilometres in geologically reasonable times. Rocks and bubbleand/or crys...
متن کاملGeology of the southeastern Eyre Mountains relevant to tenure review
Several properties within the eastern Eyre Mountains are currently undergoing tenure revue. This report provides geological information relevant to these reviews, particularly on the sequence of glacial deposits south from Kingston. The geology of the Eyre Mountains is dominated by low-grade metasedimentary rocks of the Permian Caples terrane, becoming increasingly schistose toward the northeas...
متن کاملبررسی بافتی و کانی‌شناسی کانسار روی‌ـ سرب مهدی‌آباد یزدـ ایران مرکزی
Mehdiabad Zn-Pb-Ba deposit is located 110km south-east of Yazd, in the Central Iran structural zone. The stratigraphic succession consists of three sedimentary formations of lower Creataceous age. The Sangestan formation,i.e, the lowest unit of shale and siltstone with calcarenitic interbeded layers. This unit is overlain by ankeritic massive dolomite and dolomitic limestone of Taft formation. ...
متن کاملGeology of the Central Quesnel Belt, Swift River, South-central British Columbia
In 1988 regional mapping of the central Quesnel belt (the Quesnel Project; Panteleyev, 1987, 1988; Bailey, 1988; Bloodgood, 1988) continued in the Horsefly area (Panteleyev and Hancock, 1989, this volume) and in the Swift River area, north of the Quesnel River (Figure I-l 9I). In the latter area the Mesozoic stratigraphy was mapped to north of the Quesnel-Barkerville Highway (Figure I-19-2) whe...
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ژورنال
عنوان ژورنال: Synthesis
سال: 2010
ISSN: 0039-7881,1437-210X
DOI: 10.1055/s-0030-1258325