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EVIDENCE FOR ASYMMETRIC NONVOLCANIC RIFTING AND SLOW INCIPIENT OCEANIC ACCRETION FROM SEISMIC REFLECTION DATA OF THE NEWFOUDLAND MARGIN

Shillington D.J.; Holbrook W.S.; Van Avendonk H.J.A.; Tucholke B.E.; Hopper J.R.; Louden K.E.; Larsen H.C.; Nunes G.T. (2006)

Prestack depth migrations of seismic reflection data collected around the Ocean Drilling Program (ODP) Leg 210 transect on the Newfoundland nonvolcanic margin delineate three domains: (1) extended continental crust, (2) ...
EVIDENCE FOR DEEP GROUNDWATER FLOW AND CONVECTIVE HEAT TRANSPORT IN MOUNTAINOUS TERRAIN, DELTA COUNTY, COLORADO, USA

Lazear G.D. (2006)

The Tongue Creek watershed lies on the south flank of Grand Mesa in western Colorado, USA and is a site with 1.5 km of topographic relief, heat flow of 100 mW/m2, thermal conductivity of 3.3 W m–1 °C–1, hydraulic conductivity ...
EVIDENCE FOR DIRECT MAMMALIAN FAUNAL INTERCHANGE BETWEEN EUROPE AND ASIA NEAR THE PALEOCENE-EOCENE BOUNDARY

Hooker J.J.; Dashzeveg D. (2003)

Dispersal of mammals into Europe at the beginning of the Eocene is conventionally interpreted as being solely from North America via the Greenland land bridge, as other routes were apparently unavailable because of the ...
EVIDENCE FOR EARLY MESOPROTEROZOIC ARC MAGMATISM IN THE MUSGRAVE BLOCK, CENTRAL AUSTRALIA: IMPLICATIONS FOR PROTEROZOIC CRUSTAL GROWTH AND TECTONIC RECONSTRUCTIONS OF AUSTRALIA

Wade B.P.; Barovich K.M.; Hand M.; Scrimgeour I.R.; Close D.F. (2006)

The Musgrave Block in central southern Australia separates the dominantly Paleoproterozoic North Australian Craton from the Late Archean to early Mesoproterozoic Gawler Craton in southern Australia. Geochemical and Nd ...
EVIDENCE FOR EVOLUTION OF DIAMOND CRYSTALLIZATION MEDIUM IN ECLOGITE XENOLITH FROM THE UDACHNAYA KIMBERLITE PIPE, YAKUTIA

Shatsky V.S.; Ragozin A.L.; Zetgenizov D.A.; Mityukhin S.I. (2006)

The recently obtained data on the superimposed character of diamonds in eclogite xenoliths have compelled us to consider the problem of diamond formation in the upper mantle from a new standpoint. We reported the first ...
EVIDENCE FOR EXTENSIVE PROTEROZOIC REMOBILIZATION OF THE ALDAN SHIELD AND IMPLICATION FOR PROTEROZOIC PLATE TECTONIC RECONSTRUCTIONS OF SIBERIA AND LAURENTIA

Avchenko O.V.; Frost B.R.; Chamberlain K.R.; Frost C.D. (2001)
EVIDENCE FOR HIBBINGITE-KEMPITE SOLID SOLUTION

Saini-Eidukat B.; Rudashevsky N.S.; Polozov A.G. (1998)

New occurrences of hibbingite, γ-Fe 2 (OH) 3 Cl, have been found associated with platinum-group minerals in the Noril'sk Complex, and with the Korshunovskoye iron ores of the southern Siberian platform. The Norils'k grains, ...
EVIDENCE FOR HYDROUS HIGH-MGO MELTS IN THE PRECAMBRIAN

Stone W.E.; Larson M.S.; Lesher Michael C.; Deloule E. (1997)

Prevailing petrogenetic models for Precambrian high-MgO melts such as komatiites invoke crystallization from nearly anhydrous melts (≪0.5% H2O) generated by partial melting of mantle peridotite at temperatures of (≤ 1900 ...
EVIDENCE FOR ICE VI AS AN INCLUSION IN CUBOID DIAMONDS FROM HIGH P-T NEAR INFRARED SPECTROSCOPY

Kagi H.; Lu R.; Davidson P.; Goncharov A.F.; Mao H.K.; Hemley R.J. (2000)

Near infrared absorption (NIR) spectra of natural morphologically cubic polycrystalline diamonds (cuboid) were obtained at room temperature, and the stretching plus bending combination band of molecular water was observed. ...
EVIDENCE FOR IMMISCIBILITY IN MAJORITE GARNET FROM EXPERIMENTS AT 13-15 GPA

Gasparik T. (2000)

The compositions of coexisting aluminous garnet, clinoenstatite and either jadeitic clinopyroxene or a second (silica-rich) garnet were experimentally determined in the system Na2O-CaO-FeO-MgO-Al2O3-SiO2 at 1450–1650°C and ...
EVIDENCE FOR INTENSIFICATION OF THE GLOBAL WATER CYCLE: REVIEW AND SYNTHESIS

Huntington T.G. (2006)

One of the more important questions in hydrology is: if the climate warms in the future, will there be an intensification of the water cycle and, if so, the nature of that intensification? There is considerable interest ...
EVIDENCE FOR LATE PALEOZOIC AND MESOZOIC NON-DIPOLE FIELDS PROVIDES AN EXPLANATION FOR THE PANGAEA RECONSTRUCTION PROBLEMS

Van Der Voo R.; Torsvik T.H. (2001)

Paleomagnetic pole positions have long been calculated with the assumption that the ancient geomagnetic field was purely that of a geocentric dipole, but in recent years it has become a concern that this assumption is not ...
EVIDENCE FOR LITHOSPHERIC DETACHMENT IN THE CENTRAL ANDES FROM LOCAL EARTHQUAKE TOMOGRAPHY

Schurr B.; Rietbrock A.; Asch G.; Kind R.; Oncken O. (2006)

Data from three temporary seismic networks were merged for tomographic inversion. Although the deployments did not coincide in time, spatial overlap was achieved by re-occupying existing sites. Travel times and t⁎ operators ...
EVIDENCE FOR MOLECULAR SIZE DEPENDENT GAS FRACTIONATION IN FIRN AIR DERIVED FROM NOBLE GASES, OXYGEN, AND NITROGEN MEASUREMENTS

Huber C.; Beyerle U.; Leuenberger M.; Schwander J.; Spahni R.; Weiler K.; Kipfer R.; Severinghaus J.P. (2006)

We present elemental and isotopic measurements of noble gases (He, Ne, Ar, Kr, and Xe), oxygen and nitrogen of firn air from two sites. The first set of samples was taken in 1998 at the summit of the Devon Ice Cap in the ...
EVIDENCE FOR MONAZITE- , BARITE- , AND AGMNO4 (DISTORTED BARITE)-TYPE STRUCTURES OF CASO4 AT HIGH PRESSURE AND TEMPERATURE

Crichton W.A.; Parise J.B.; Antao S.M.; Grzechnik A. (2005)

Using laser-heated diamond-anvil cells, we have observed CaSO4 undergoing phase transitions from its ambient anhydrite structure to the monazite type, and at highest pressure and temperature to crystallize in the barite-type ...
EVIDENCE FOR RAPID ENVIRONMENTAL CHANGES IN LOW LATITUDES DURING THE LATE SILURIAN LAU EVENT: THE BURGEN-1 DRILLCORE, GOTLAND, SWEDEN

Calner M.; Eriksson M.J. (2006)

Erosional outliers are an important component of the Ludlow (Late Silurian) stratigraphy of Gotland, Sweden. However, due to the poor degree of exposure, outcrop studies have not revealed a detailed section from any of ...
EVIDENCE FOR REACTIVATION OF EOCENE JOINTS AND PRE-EOCENE FOLIATION PLANES IN THE OKANAGAN CORE-COMPLEX, BRITISH COLUMBIA, CANADA

Eyal Y.; Feinstein S.; Osadetz K.G. (2006)

We studied the brittle deformational history of the Okanagan metamorphic core complex, and its hanging wall carapace, in the Canadian Cordillera, in southern British Columbia by an extensive structural investigation at ...
EVIDENCE FOR SOLAR NEBULA SIGNATURES IN THE MATRIX OF THE ALLENDE METEORITE

Brenker F.E.; Palme H.; Klerner S. (2000)

Carbonaceous chondrites of type 3 (e.g. Allende) are among the most primitive meteorites. They contain components that formed prior to the accretion of a parent asteroid and thus record conditions of the ambient nebular ...
EVIDENCE FOR SUBDUCTION-RELATED COMPONENTS IN THE SUBCONTINENTAL MANTLE FROM LOW 3HE/4HE AND 40AR/36AR RATIO IN MANTLE XENOLITHS FROM FAR EASTERN RUSSIA

Yamamoto J.; Kaneoka I.; Nakai S.; Kagi H.; Prikhod'ko V.; Arai S. (2004)

By applying both vacuum crushing and stepwise heating methods for the extraction of the noble gases, we have discovered ³He/⁴He ratios much lower than the atmospheric ratio (∼0.3 RA; RA is the atmospheric ³He/⁴He ratio of ...
EVIDENCE FOR SVECONORWEGIAN (GRENVILLIAN) MAGMATIC ACTIVITY IN THE NORTHWESTERN BALTIC SHIELD

Arzamastsev A.A.; Arzamastseva L.V.; Fedotov Zh.A.; Montero P.; Bea F.; Travin A.V. (2006)

The crustal structure in the Baltic Shield is determined by a system of geological blocks, which formed at different evolutionary stages of this largest stable Precambrian domain. Cratonization of the Archean Karelian, ...

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