Beloc, Haiti,
KT boundary site

|

|
SEM backscatter image of tektite core. Dark
areas are CaO poor, the light streaks are Ca and P
(phosphorus) rich. The lighest streak contains up
to 5% P2O5, and a grain of CaP04. [hres
image]
|

|
Same Core, enhanced contrast
|
|

|
Polished slab of the K/T boundary ejecta layer with
numerous tektite cores that still contain glass (detail
above). The layer is graded, rather because of gravity flow
depositional mechanism of the layer and probably not through
differential settling through the atmosphere and
watercolumn. The slab shown is from the B-locality (see
map). With the localities discovered earlier by Maurasse,
this is the only one of many that has yieldede glass
remains, usually in the core of the tektites
|
|
More about tektites
here
|