Hello Listers and Lunar Junkies :)

I came across this article about Lunar meteorites and I have to say its a good 
read on explaining the conditions the inner solar system might have gone 
through with the help of Lunar meteorite samples. Now all we need is to have a 
first Lunar meteorite fall and it has be happen around NYC :) preferably 
Brooklyn while I am walking home from the subway :)

Shawn Alan
IMCA 1633
eBay Store
http://www.ebay.com/sch/ph0t0phl0w/m.html?
http://www.meteoritefalls.com/
 
 AN EXTENDED EPISODE OF EARLY BOMBARDMENT IN THE INNER SOLAR SYSTEM:
EVIDENCE FROM LUNAR SAMPLES AND METEORITES. 
M. D. Norman1,2 and A. A. Nemchin3,1
Research School of Earth Sciences, Australian National University, Canberra ACT 
0200 Australia([email protected]), 
3Department of Applied Geology, Curtin University of Technology, Perth WA 
6845Australia ([email protected]).
 
 Introduction: 
A spike in the flux of asteroid-sizebodies traversing the inner Solar System 
and impacting
the terrestrial planets at 3.9 Ga has become a keystone
of recent models describing planetary dynamics [1],
the chronology of planetary surfaces [2] and assessments
of the potential habitability of early terrestrial
environments [3,4]. Lunar samples provided the initial
observational data that motivated this idea [5, 6], and
the lunar cratering record now serves as a reference
frame for the cratering chronology of Mars and inner
solar system [7].
The absence of lunar impact melt breccias with ages
between ~4.4 and 3.9 Ga has long been cited as evidence
favoring a relatively low average impact flux
during the interval between planetary accretion and the
formation of many if not all of the lunar basins during
a relatively brief episoce of late heavy bombardment
from ~3.8 to 4.0 Ga [3]. However, large impact events
on the Moon with ages ranging from 4.1-4.3 Ga have
been inferred from recent dating of lunar zircons [8, 9]
from previously unrecognized varieties of lunar impact
melt breccias [10, 11], from clasts in fragmental lunar
breccias [12] and from metamorphic lunar breccias
(granulites) [13]. Here we summarize the lunar sample
evidence for pre-cataclysm (i.e. older than 3.9 Ga)
impact events on the Moon, and suggest that the basinforming
epoch likely spanned a significantly longer
period of time than implied by the Cataclysm Hypothesis.
 
 
http://www.lpi.usra.edu/meetings/earlymars2012/pdf/7051.pdf
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