نتایج جستجو برای: weak rocks

تعداد نتایج: 162522  

Journal: :The Journal of experimental biology 2004
Damian O Elias Andrew C Mason Ronald R Hoy

The jumping spider Habronattus dossenus Griswold 1987 (Salticidae) communicates using seismic signals during courtship and can be found on rocks, sand and leaf litter. We examined the filtering properties of, and tested the efficacy of male courtship signals on, these natural substrates. These substrates have drastically different filtering properties at the distances at which the males court. ...

2002
Z. Xu B. C. Gahan

High power carbon dioxide lasers have successfully been used in drilling or cutting ngineering materials such as metals, polymers and ceramics over the years. Can a arbon dioxide laser be used to efficiently drill different rocks in a deep gas well? esearch sponsored by US Department of Energy has been carried out to answer this uestion. This paper will report the study results of using a super...

2015
Jonathan T. Uhl Shivesh Pathak Danijel Schorlemmer Xin Liu Ryan Swindeman Braden A. W. Brinkman Michael LeBlanc Georgios Tsekenis Nir Friedman Robert Behringer Dmitry Denisov Peter Schall Xiaojun Gu Wendelin J. Wright Todd Hufnagel Andrew Jennings Julia R. Greer P. K. Liaw Thorsten Becker Georg Dresen Karin A. Dahmen

Slowly-compressed single crystals, bulk metallic glasses (BMGs), rocks, granular materials, and the earth all deform via intermittent slips or "quakes". We find that although these systems span 12 decades in length scale, they all show the same scaling behavior for their slip size distributions and other statistical properties. Remarkably, the size distributions follow the same power law multip...

2005
J. Pehl H.-R. Wenk

Preferred orientation in granitic mylonites from the Santa Rosa mylonite zone in Southern California is investigated with time-of-flight neutron diffraction. Quartz and biotite display strong preferred orientation, whereas, feldspar alignment is weak. For quartz, a c-axis maximum in the intermediate fabric direction is consistent with dynamic recrystallization. Pole figures for positive and neg...

2017
V. E. D. OBOT

We performed a ground level geomagnetic survey of Greene County, Ohio in the fall of 1976. The geomagnetic map showed a positive magnetic anomaly running from the northwestern section to the southeastern section of the county while the remainder of the map was relatively undisturbed. We analyzed the localized anomaly of the southeastern section by the Peters methods and by fitting to the model ...

2008
Michiel van Dongen Andrew G. Tomkins Roberto F. Weinberg

The Ok Tedi Complex hosts a world-class porphyry copper-gold deposit. Samples from the Ok Tedi Complex and the neighbouring Mount Ian Complex were analyzed for major and trace elements using XRF and HR-ICP-MS, and the isotopic composition of S in sulphides was analyzed by Elemental Analyzer. Major element geochemistry indicates that both complexes are alkaline and contain rocks ranging in compo...

2017
Nicoletta Christina Browne

Over summer 2017, I continued my research on dikes emplaced during the waning stages of the Neoproterozoic-Ordovician Ross Orogen, a continental arc along the present day location of the Transantarctic Mountains in Antarctica. The dikes intrude calc-alkaline plutons constituting the main intrusive phase as well as metasedimentary rocks formed during early stages of orogenesis. These dikes compr...

Journal: :Science 2016
Joanna V Morgan Sean P S Gulick Timothy Bralower Elise Chenot Gail Christeson Philippe Claeys Charles Cockell Gareth S Collins Marco J L Coolen Ludovic Ferrière Catalina Gebhardt Kazuhisa Goto Heather Jones David A Kring Erwan Le Ber Johanna Lofi Xiao Long Christopher Lowery Claire Mellett Rubén Ocampo-Torres Gordon R Osinski Ligia Perez-Cruz Annemarie Pickersgill Michael Poelchau Auriol Rae Cornelia Rasmussen Mario Rebolledo-Vieyra Ulrich Riller Honami Sato Douglas R Schmitt Jan Smit Sonia Tikoo Naotaka Tomioka Jaime Urrutia-Fucugauchi Michael Whalen Axel Wittmann Kosei E Yamaguchi William Zylberman

Large impacts provide a mechanism for resurfacing planets through mixing near-surface rocks with deeper material. Central peaks are formed from the dynamic uplift of rocks during crater formation. As crater size increases, central peaks transition to peak rings. Without samples, debate surrounds the mechanics of peak-ring formation and their depth of origin. Chicxulub is the only known impact s...

2002
T. Vanorio M. Prasad D. Patella A. Nur

This paper summarizes results of a study of porosity, permeability, microstructure and acoustic properties of volcanic and pyroclastic rocks fromCampi Flegrei (CF) andMt. Etna (ET), Italy. We have measured the hydraulic, transport and acoustics properties of 28 room-dry samples at ambient conditions, 25 room-dry samples under confining pressure (up to 60 MPa) and 5 brine saturated samples under...

2011
J. B. Wright

85 The physiography of the area is dominated by glaciated landforms carved in gneiss of the Fiordland Complex. The gneiss is generally dioritic, with gradations to quartzo-feldspathic and amphibolitic varieties, and is cut by mainly barren pegmatite veins; epidote is abundant. The rocks commonly show signs of post-consolidational shearing and crushing. There is a well defined zone of strongly c...

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