scholarly journals A search for shocked quartz grains in the Allerød‐Younger Dryas boundary layer

2015 ◽  
Vol 50 (3) ◽  
pp. 483-498 ◽  
Author(s):  
Annelies Hoesel ◽  
Wim Z. Hoek ◽  
Gillian M. Pennock ◽  
Knut Kaiser ◽  
Oliver Plümper ◽  
...  
Keyword(s):  
Boundary Layer ◽  
Younger Dryas ◽  
Shocked Quartz ◽  
Quartz Grains

Shocked quartz grains from the Målingen structure, Sweden-Evidence for a twin crater of the Lockne impact structure

2014 ◽  
Vol 49 (6) ◽  
pp. 1076-1082 ◽  
Author(s):  
C. Alwmark ◽  
S. Alwmark-Holm ◽  
J. Ormö ◽  
E. Sturkell
Keyword(s):  
Impact Structure ◽  
Shocked Quartz ◽  
Quartz Grains

Microscopic planar features in quartz from Scollard Canyon, Alberta, and the Cretaceous–Tertiary boundary event

1988 ◽  
Vol 25 (9) ◽  
pp. 1530-1534 ◽  
Author(s):  
R. A. F. Grieve ◽  
J. Alexopoulos
Keyword(s):  
Continental Margin ◽  
Crystalline Rocks ◽  
Meteorite Impact ◽  
Isotopic Data ◽  
Near Surface ◽  
Deformation Features ◽  
Shocked Quartz ◽  
Quartz Grains ◽  
Geologic Processes ◽  
Basaltic Material

Quartz grains separated from the Cretaceous–Tertiary (K/T) boundary clay at Scollard Canyon, Alberta, have prominent, microscopic planar features. These occur in 15–30% of the grains from the lower 1.5 cm of the boundary clay. They commonly correspond to the ω and π orientations found at known meteorite impact sites and differ from deformation features produced by other dynamic geologic processes. Basal planar features, however, are absent here and at other K/T sites. One possible explanation is that quartz at boundary sites is an incomplete sample of shocked quartz from the postulated K/T impact and unshocked detrital quartz. The source of the shocked quartz most likely was close to the point of impact and near surface. This and previous isotopic data suggest the K/T target site contained a relatively thin upper unit of quartz-bearing crystalline rocks overlying basaltic material, corresponding possibly to thinned continent or a continental margin.

scholarly journals Reply to Ives and Froese: Regarding the impact-related Younger Dryas boundary layer at Chobot site, Alberta, Canada

2013 ◽  
Vol 110 (41) ◽  
pp. E3900-E3900 ◽  
Author(s):  
J. H. Wittke ◽  
T. E. Bunch ◽  
K. B. Tankersley ◽  
I. R. Daniel ◽  
J. B. Kloosterman ◽  
...  
Keyword(s):  
Boundary Layer ◽  
Younger Dryas ◽  
The Impact

A search for shocked quartz grains and impact ejecta in early Silurian sediments on Gotland, Sweden

1994 ◽  
Vol 131 (3) ◽  
pp. 361-367 ◽  
Author(s):  
Birger Schmitz ◽  
Lennart Jeppsson ◽  
Johan Ekvall
Keyword(s):  
Lateral Spreading ◽  
Asteroid Impact ◽  
The Earth ◽  
Planar Shock ◽  
Impact Ejecta ◽  
Single Grain ◽  
Shocked Quartz ◽  
Impact Events ◽  
Impact Origin ◽  
Quartz Grains

AbstractAll bentonite and bentonite-resembling layers thicker than a few millimetres from a 120m-thick Early Silurian sequence on Gotland, Sweden, were searched for shocked quartz grains of comet or asteroid impact origin. Although more than 200000 quartz grains from 86 bentonite samples were studied, not one single grain with multiple planar shock features was found. The studied sequence represents sedimentation during a period of about 2 million years. Impact frequencies, estimated from the cratering record and astronomical observations, indicate that during a 2-myr- period on average 20 comet or asteroid bodies larger than 0.5 km in diameter strike the Earth. The number of smaller impacting bodies is many times higher. In the light of this high frequency of impacts, the absence of any shocked-quartz-bearing fallout layer in our sequence indicates that lateral spreading of such ejecta is relatively restricted during small- and medium-scale impact events.The results also show that shocked quartz in general is absent or extremely rare in volcanic ash. This strengthens the case for an impact-related origin of shocked quartz grains in the Cretaceous–Tertiary boundary days.

Shocked quartz grains at the Cretaceous-Tertiary boundary

1988 ◽  
Vol 75 (6) ◽  
pp. 307-308 ◽  
Author(s):  
R. Seitz ◽  
B. F. Bohor
Keyword(s):  
Shocked Quartz ◽  
Quartz Grains

scholarly journals Characterization of shocked quartz grains from Chicxulub peak ring granites and shock pressure estimates

2020 ◽  
Vol 55 (10) ◽  
pp. 2206-2223
Author(s):  
Jean‐Guillaume Feignon ◽  
Ludovic FerriÈre ◽  
Hugues Leroux ◽  
Christian Koeberl
Keyword(s):  
Shock Pressure ◽  
Shocked Quartz ◽  
Quartz Grains

scholarly journals PDF orientations in shocked quartz grains around the Chicxulub crater

2008 ◽  
Vol 43 (4) ◽  
pp. 745-760 ◽  
Author(s):  
Yoichiro NAKANO ◽  
Kazuhisa GOTO ◽  
Takafumi MATSUI ◽  
Ryuji TADA ◽  
Eiichi TAJIKA
Keyword(s):  
Chicxulub Crater ◽  
Shocked Quartz ◽  
Quartz Grains

Shocked quartz grains in rhyolitic bentonites

2010 ◽  
Vol 21 (S1) ◽  
pp. 133-134
Author(s):  
H. J. Hansen ◽  
P. Toft ◽  
Jinnan Tong
Keyword(s):  
Shocked Quartz ◽  
Quartz Grains

Shocked quartz grains in the early Cambrian Vakkejokk Breccia, Sweden—Evidence of a marine impact

2018 ◽  
Author(s):  
Carl Alwmark ◽  
Jens Ormö ◽  
Arne T. Nielsen
Keyword(s):  
Early Cambrian ◽  
Shocked Quartz ◽  
Quartz Grains

RAPID COMMUNICATIONS Complex quartz growth histories in granite revealed by scanning cathodoluminescence techniques

1997 ◽  
Vol 134 (4) ◽  
pp. 549-552 ◽  
Author(s):  
R. S. D'LEMOS ◽  
A. T. KEARSLEY ◽  
J. W. PEMBROKE ◽  
G. R. WATT ◽  
P. WRIGHT
Keyword(s):  
Boundary Layer ◽  
Electron Microscope ◽  
Low Intensity ◽  
Collector System ◽  
Limited Variation ◽  
Progressive Growth ◽  
Melt Composition ◽  
Quartz Grains ◽  
Mixing Behaviour ◽  
Scanning Electron

A scanning electron microscope based cathodoluminescence technique utilizing a novel collector system reveals complex internal heterogeneities within granitic quartz grains. The technique overcomes the low intensity and limited variation in cathodoluminescence generated by quartz, which hamper conventional cathodoluminescence analysis. Detailed images of zoning patterns in quartz are comparable to those observed in minerals such as feldspar, and attributed to a combination of progressive growth, boundary layer effects and mineral–melt disequilibria produced during fluctuations in melt composition and temperature during the crystallization interval. We attribute such mineral–melt disequilibria to open system, mixing behaviour in the granite plutons sampled.

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