From mid-Ordovician ∼470 Myr-old limestone >100 fossil L-chondritic meteorites have been recovered, representing the markedly enhanced flux of meteorites to Earth following the breakup of the L-chondrite parent body. Recently one anomalous meteorite, Österplana 065 (Öst 65), was found in the same beds that yield L chondrites. The cosmic-ray exposure age of Öst 65 shows that it may be a fragment of the impactor that broke up the L-chondrite parent body. Here we show that in a chromium versus oxygen-isotope plot Öst 65 falls outside all fields encompassing the known meteorite types. This may be the first documented example of an 'extinct' meteorite, that is, a meteorite type that does not fall on Earth today because its parent body has bee...
This thesis aims at reconstructing events in the solar system, mainly collisional events in the aste...
11siWe have reconstructed the distribution of extraterrestrial chrome spinels in a marine limestone ...
AbstractA large abundance of L-chondritic material, mainly in the form of fossil meteorites and chro...
From mid-Ordovician ∼470 Myr-old limestone >100 fossil L-chondritic meteorites have been recovered, ...
About a quarter of all meteorites falling on Earth today originate from the breakup of the L-chondri...
Mid-Ordovician fossil meteorites found in the Thorsberg quarry, southern Sweden, are believed to hav...
We show that Earth’s sedimentary strata can provide a record of the collisional evolution of the ast...
© 2017 Macmillan Publishers Limited, part of Springer Nature. All rights reserved. Most meteorites t...
AbstractAbout a quarter of all meteorites falling on Earth today originate from the breakup of the L...
© The Author(s), 2014. This article is distributed under the terms of the Creative Commons Attributi...
Previous studies of limestone beds of mid-Ordovician age from both Sweden and China show that the Ea...
This thesis deals with signatures in sediments on Earth related to the L-chondrite parent body break...
The meteoritic material falling on Earth is believed to derive from large break-up or cratering even...
Abundant fossil meteorites in marine, condensed Lower Ordovician limestones from Kinnekulle, Sweden,...
The Brunflo fossil meteorite was found in the 1950s in mid-Ordovician marine limestone in the Grde q...
This thesis aims at reconstructing events in the solar system, mainly collisional events in the aste...
11siWe have reconstructed the distribution of extraterrestrial chrome spinels in a marine limestone ...
AbstractA large abundance of L-chondritic material, mainly in the form of fossil meteorites and chro...
From mid-Ordovician ∼470 Myr-old limestone >100 fossil L-chondritic meteorites have been recovered, ...
About a quarter of all meteorites falling on Earth today originate from the breakup of the L-chondri...
Mid-Ordovician fossil meteorites found in the Thorsberg quarry, southern Sweden, are believed to hav...
We show that Earth’s sedimentary strata can provide a record of the collisional evolution of the ast...
© 2017 Macmillan Publishers Limited, part of Springer Nature. All rights reserved. Most meteorites t...
AbstractAbout a quarter of all meteorites falling on Earth today originate from the breakup of the L...
© The Author(s), 2014. This article is distributed under the terms of the Creative Commons Attributi...
Previous studies of limestone beds of mid-Ordovician age from both Sweden and China show that the Ea...
This thesis deals with signatures in sediments on Earth related to the L-chondrite parent body break...
The meteoritic material falling on Earth is believed to derive from large break-up or cratering even...
Abundant fossil meteorites in marine, condensed Lower Ordovician limestones from Kinnekulle, Sweden,...
The Brunflo fossil meteorite was found in the 1950s in mid-Ordovician marine limestone in the Grde q...
This thesis aims at reconstructing events in the solar system, mainly collisional events in the aste...
11siWe have reconstructed the distribution of extraterrestrial chrome spinels in a marine limestone ...
AbstractA large abundance of L-chondritic material, mainly in the form of fossil meteorites and chro...