Injected sandstones occurring in the Kimmeridgian of NE Scotland along the bounding Great Glen and Helmsdale faults formed when basinal fluids moved upward along the fault zones, fluidizing Oxfordian sands encountered at shallow depth and injecting them into overlying Kimmeridgian strata. The orientation of dykes, in addition to coeval faults and fractures, was controlled by a stress state rela...

In the upper Subansiri District of Arunachal Pradesh, India, Higher Himalayan Crystallines are exposed in and around Taliha and the outcrop of MCT in the immediate south of Taliha is recognizable with the development of tourmaline bearing leucogranite dykes representing melting of the crustal rocks. The gneisses of the Taliha area consist of mainly quartz, mica, K-feldspar and garnet. The Quart...

* Corresponding author 16 Dr. Gary A. Dykes 17 Food Science Australia 18 PO Box 3312 19 Tingalpa DC, Queensland, 4173, Australia 20 Phone: +61 7 3214 2037 21 Fax: +61 7 3214 2150 22 Email: [email protected] 23 AC CE P ED Copyright © 2009, American Society for Microbiology and/or the Listed Authors/Institutions. All Rights Reserved. Appl. Environ. Microbiol. doi:10.1128/AEM.02232-08 AEM Accept...

The major and trace element characteristics of the clinopyroxene from two generations dykes, dolerite olivine dykes Western Dharwar Craton were investigated by using electron microprobe LA–ICPMS. in show a compositional zoning with Mg# decreasing core to rim (85 51) Cr2O3 contents decrease towards rim. rare earth (REE) pattern shows lower concentrations REEs compared dolerites are devoid compos...

The Sungun Cu-Mo porphyry deposit forms part of the Ahar–Arasbaran Magmatic Belt (AAMB). Its host Miocene stock is quartz monzonitic in composition and cut by intermediate dykes that post-date mineralization. These contain pyroxene enclaves ambiguous origin. Dykes microdiorite are observed within diorite dykes, whereas later three different kinds (diorite, hornfels) sizes between 1 10 cm. Encla...

S U M M A R Y In the early stages of continental rifting, extension takes place by normal faulting, while in mature continental rifts dyke intrusion dominates. Little is known about the nature of the transition between fault-controlled and dyke-controlled extension or about the processes in an intermediate setting. Here, we present observations of the temporal and spatial evolution of surface d...