Are volcanic glasses and tektites of the same origin ?

 

Norbert Brügge, Germany

Dipl.-Geol.

 

It is urgently necessary to brake the currently raging impact crater hysteria. With the help of meanwhile established criteria many impact-events became postulated, mostly too quickly and not sufficient examined. All endogenous possibilities were ignored. Still worse, multiple is worked only with satellite pictures. Alone already the origin of so-called tektites or impact glasses is an important discussion. The question is, are volcanic glasses and tektites of the same origin ? Yes, I believe it. It is a disruptive theme, that is conceded.
 

All of natural glasses found on the earth are from amorphous structure and have a high to very high SiO2 capacity. They are divided in four classes: Tektite, impact glasses and volcanic glasses. However until today is not clarified, whether the practised division of glasses is right to such classes. There is no safety, that the locations of glass finds can be associated e.g. with impact structures, or such are the originally location of glasses. For the existence of tektites - emerged by an impact event - there is practically no proofs. It has also up to now not been successful, to prove a satisfactory chemical equality between supposed target rocks and glass locations. It is not impossible, that most glasses found on the earth are volcanic of origin.

Besides is not finally clarified whether such "typical" criteria for an impact, like the high temperature and high pressure minerals (e.g. Coesite, Stishovite), shatter cone structures, planar deformations in quartz grains or breccias (Suevite) also emerged by very high-dynamic volcanic events. Various localities, which were classified as impact structures, would be then endogenous origin. Striking examples for an uncertain origin are the Vredefort and Popigai structures.
What kind of enormous dynamics by the explosion of a super - volcano is to be expected, the idea would be, that the magma - chamber under the Yellow Stone Park explodes again. The thrown out masses would be exposed tremendous changes.
During an explosion of the powerful magma chamber a dynamic would emerge presumably, which we do not know up to now. Why should a such powerful explosion not be comparable the dynamics by an impact?


Popigai structure, Siberia



Vredefort structure, RSA


The greatest question is however:
 

Can document the "flying glasses" furious volcanic outbreaks ? For that reason, if we believe to know already everything, then we make a mistake. The known example for the unsolved origin of a glass is the Libyan Desert Glass (LDG or LDSG). It has the highest SiO2 capacity of all natural glasses and is surely also no an impact glass.

Tektite and impact glasses should be of equal origin. Tektite should be impact glasses, which are found far from the origin location of the impact. In Europe are found the green Moldavite. Tektite of Indochina and Australia are mostly black, some forms are dumbbell-shaped, in part discus-shaped and flattened, also round and spherical in many forms. Tektite have therefore often an aerodynamic form, also a scarred surface with melted structures. The kind of the physical characteristics the tektite resemble of the volcanic Obsidian (the most known volcanic glass).
Tektite should differ from volcanic glasses by a higher SiO2 capacity as well as by an extremely poor water capacity. Also so characteristic inclusion of micro-crystals in volcanic glasses should be missing.

To improve the scarce data base of H2O content in tektites and impact glasses, University Wien (Prof. KOEBERL) analyzed 26 tektites from all four strewn fields and 25 impact glass samples for their H2O content. The results show that the tektites have H2O contents ranging from 0,002 to 0,030 wt% (av. 0,014 ± 0,008 wt%). Ivory Coast tektites have the lowest H2O abundances (0,002-0,003 wt%); the Muong Nong-type indochinites and some North American tektites having the highest contents (up to approx. 0,03 wt%). Glasses from the Aouelloul and Zhamanshin craters have low H2O content (0,008 to 0,063 wt%). Libyan Desert Glasses have higher H2O content (approx. 0,11 wt%). Data confirm that all tektites found on land have very low H2O contents (<0,03 wt% H2O), while impact glasses have slightly higher H2O contents. Both glass types are very dry compared to volcanic glasses. Obsidians have water content higher as 0,20 wt%.
It becomes clear, that between all glasses in the capacity of water no separation is to be recognized.

Are this postulated differences between impact glasses/tektites on one hand and volcanic glasses on the other hand a so important characteristic ?
Emerged this differences by differently conditions before and during an eruption. Sure is, that all natural glasses - also tektite and impact glasses - can be associated with volcanic rock types. Extreme exceptions are the LDG, the Urengoite and the Aouelloul glass with very high or extreme high SiO2 content.


 

 

Short Lesson

There are two types of magmatic (igneous) rocks
There is a wide variety of igneous rocks types but only a few basic types of magma, because the asthenosphere and upper mantle have a fairly uniform composition.
Plutonic rocks (intrusive) form when the magma cools slowly beneath the surface, while eruptive volcanic rocks (extrusive) form when magma reaches the surface and cools rapidly.
The mostly igneous rocks are composed of approximately 50 - 80 wt% SiO2, 10 - 20 wt% Al2O3, 1 - 2 wt% MgO, 1 - 5 wt% FeO, 1 - 5 wt% CaO, 1 - 5 wt% K2O, 1 - 2 wt% Na2O.
Igneous rocks with a capacity of < 90 wt% of SiO2 (and that is the predominant part) can be classified in a QAPF - diagram of the presence from light parts in the mixture (felsic) in the rocks. This happens for plutonite and eruptiva in separate triangles after that equal principle.

1. Volcanic glasses
Volcanic glass emerges from quick cooling of gas-poor eruptiva. Volcanic glass can refer to any of several types of vitreous igneous rocks. Most commonly, it refers to Obsidian, a rhyolitic glass with high silica content. Rarer are
Tachylite, a basaltic glass with relatively low silica content.
Palagonite, a basaltic glass with relatively low silica content.
Pele's hair, threads or fibers of volcanic glass, usually basaltic.
Pele's tears, tear-like drops of volcanic glass, usually basaltic.
Limu o Pele, thin sheets and flakes of brownish-green to near-clear volcanic glass, usually basaltic.

By virtue of the quick cooling can increase no regular crystals. The glass has with it a chaotic, amorphous structure.
The most volcanic glasses have a SiO2 capacity between 50 and 80 wt%, and are arranged in the rhyolith, trachytic, dacitic, andesitic and basaltic families of eruptive rocks.
Volcanic glasses can contain inclusions of radial increased structures, so-called spherolithes. These minerals, mostly feldspars or Cristobalit (a high temperature modification of quartz) increased spherical at a kernel in the surrounding melt, until stopped this process the cooling.



2. Tektite glasses
are similar in chemistry to terrestrial volcanic glass.
From the geochemical point of view the chemical analysis characterizes at all the tektite glasses as rhyolitic or dacitic (wie beim Obsidian auch). The melt is oversaturated in SiO2 and molecular Al2O3 and their concentration is but clearly greater than the sum of Na2O + K2O + CaO in comparison to the Obsidian. The tektite glasses are peraluminous.
Also by the alkali-lime index (Na2O + K2O) and CaO in terms of SiO2 the tektite glasses are determined characterized by a rhyolitic composition.
Glasses were formed from a rhyolitic or dacitic volcanic melt. They are characterized as high polymerized network glasses in with respect to their glass structure by the chemical composition, (especially by the SiO2-content), as high polymerized network glasses.






3. Impact glasses
Glasses - as the result of an impact classified - have an extensive spectrum of their composition. Accordingly the silica/alkaline index are some glasses nearby the Obsidian or the Tektites. Other with an unusually high SiO2 - part have an affinity to the orthomagmatic-hydrovolcanic emerged LDG. Most glasses can be associated however with volcanic rocks.
 

Between Obsidian - the most frequent volcanic glass - and the tektites as well as impact glasses gives however a striking difference of chemistry.
The part of Na2O+K2O is at the volcanic Obsidian approximately doubly so much as at tektitic glasses. That means, that the Obsidian is emerged by rhyolitic-trachytic eruptions, and the tektites (incl. Moldavite) is emerged by rhyolitic-dacitic eruptions. It is not a feature to separate both.
Also is interesting, that the glasses of the El'gygytgyn - classified as impact glasses - have a clear affinity to the Obsidian.
With a great amount of chemical analyses of different glaziers (incl. mikrotektites) the thesis of the volcanic origin of all glasses can be proven (at least of the tektite). The here presented analyses are freely accessible in the internet.
An important source to the microtektites here: www.univie.ac.at/geochemistry/koeberl/publication-list/256-Mikrotektites-GCA2004.pdf

1. Volcanic glass
Oxide   (wt%) Hawaii glass
SiO2 51,80
Al2O3 10,20
TiO2 2,70
FeO 12,0
MgO 8,00
CaO 8,60
Na2O 1,60
K2O

0,40


Recently Hawaiian volcanic glass (Limu o Pele)


Volcanic "Pele's tears" (Hawaii)
 
 Obsidian (world wide) Type: Rhyolitic-trachytic Age: ?
The Obsidian is the classic worldwide occurring volcanic glass. Obsidian is a type of naturally-occurring glass formed as an extrusive igneous rock. It is produced when felsic lava erupted from a volcano cools rapidly through the glass transition temperature and freezes without sufficient time for crystal growth. Obsidian is commonly found within the margins of rhyolitic lava flows known as obsidian flows, where cooling of the lava is rapid.
Obsidian is mineral-like, but not a true mineral because it is not crystalline. It is sometimes classified as a mineraloid. While a rock like basalt is dark because of ferromagnesian enrichment, obsidian consists mainly of SiO2 (silicon dioxide), usually 70% or more. The most Obsidians are arranged in the trachytic and rhyolith families of eruptive rocks. Rhyolithe are the volcanic equivalents of the granites. Because obsidian is metastable at the earth's surface (over time the glass becomes fine-grained mineral crystals), no obsidian has been found that is older than Cretaceous age. Obsidian has a chaotic, amorphous structure. However can be embedded single crystals in more or less great quantities in the glassy mass. Obsidian glasses can contain inclusions of radial increased structures, so-called spherolithes. These minerals, mostly feldspars or Cristobalit (a high temperature modification of quartz) increased spherical at a kernel in the surrounding melt, until stopped this process the cooling. The breakdown of obsidian is accelerated by the presence of water. Obsidian contain approx. 0.2 -0.5 wt% water.
While pure obsidian is usually dark in appearance, the colour varies depending on the presence of impurities. Iron and magnesium typically give the obsidian a dark green to brown to black colour. A very few samples are nearly clear. In some stones, the inclusion of small, white, radially clustered crystals of cristobalite in the black glass produce a blotchy or snowflake pattern (snowflake obsidian). It may contain patterns of gas bubbles remaining from the lava flow, aligned along layers created as the molten rock was flowing before being cooled. These bubbles can produce interesting effects such as a golden (sheen obsidian) or rainbow sheen (rainbow obsidian).
Obsidian can be found in many locations around the world which have experienced rhyolitic eruptions. Obsidian can be found in North America, Mexico, Peru, Iran, Armenia, Turkey, Italy, Greece and Scotland.
The colours in obsidian result from the oxidation state of the chemical elements within the tiny minerals that are finely dispersed in the glass. Black colour results chiefly from magnetite, Fe304. If the obsidian is highly oxidized, then the glass may contain hematite, which provides a reddish hue. Variations in the oxidation state of the iron (Fe) varieties imparts a slight greenish hue. Some obsidian is banded, a consequence of oxidation on a flow surface being folded into the lava as it continues to move.
 
Oxide  (wt%)

Shahryri (Iran)

 Lipari Islands (Italia)

 Yellowstone (USA)

 New Mexico(USA)
Nadooshan et al., 2007 Hunt et al., 1998 Hatch et al., 1972 Hölzle-Y., 1992 Rose et al.
range (12) average  range (45) average average (?) average (?) average (?)
SiO2 62,75 79,29 70,90 73,59 75,61 74,26 76,78 75,00 76,40
Al2O3 8,76 12,02 10,73 12,76 13,67 13,16 12,09 12,50 12,70
TiO2 0,09 0,12 0,11 0,03 0,14 0,08 0,08 0,11 0,10
FeO 0,66 1,35 0,96 1,27 1,67 1,50  2,61 1,00 0,58
MgO 0,02 0,23 0,07 0,02 0,07 0,04 0,10 0,03 0,40
CaO  ? ?  ? 0,66 0,80 0,74 0,57 0,60 0,30
Na2O 3,58 4,10 3,80 2,44 4,27 3,84 3,79 2,90 4,10
K2O 3,48 4,15 4,00 5,00 5,33 5,13 4,93 5,10 4,57





Dark bands in the brownish matrix






 Apache Tears (Arizona, USA) Type: Rhyolitic ?  Age: ?
Apache Tears are Obsidians.



 


 Colombianite (Colombia, Peru)  Type: Rhyolitic ? Age: 15 Ma ? (Miocene)
The Columbianite are unusual glasses. They become mainly found in the region of the Orinoco river, Colombia. The glasses were counted up to now among the tektite, because the structure at the surface is similar to tektites. The chemical composition however clearly should correspond the Obsidians.





 



 
 Libyan Desert Glass (Egypt)

Type: ?

 Age: 28 -29 Ma (Oligocene)
The Libyan Desert Glass is classified still always as tektite or impact glass. That is nonsense. The LDG can be arranged in no known class up to now. No natural glass has a SiO2 content with more than 95 wt%. It is in all probability an orthomagmatic-hydrovolcanic glass and is unique on the world up to now. See my report here
 
Oxide (wt%)

Gucsik at al., 2004

 Giuli et al., 2003 Guzzafame et al., 2009

bright variety

dark variety

 bright bright dark streak yellow green
range (8) average range (6) average single single single single single single
SiO2 96,40  98,10 97,20 92,80 97,80 95,97 98,44 98,27 95,85 97,19 96,71 92,52
Al2O3 0,49 1,70 1,12 0,07 2,39 1,30 0,55 1,30 1,48 0,86 1,19 1,88
TiO2 0,06 0,38 0,21 0,15 0,85 0,36 0,08 0,17 0,18 0,07 0,20 0,81
MnO 0,08 0,44 0,24 0,09 0,92 0,31 0,01 0,01 0,02 - - 0,03
FeO 0,04 0,55 0,22 0,09 1,06 0,36 0,09 0,12 0,98 0,06 0,14 2,09
MgO 0,09 0,51 0,32 0,03 0,58 0,32 0,01 0,01 1,38 0,08 0,11 0,13
CaO 0,04 0,18 0,13 0,09 1,88 0,47 0,01 0,01 0,08 0,08 0,06 0,85
Na2O 0,04 0,43 0,22 0,03 0,40 0,21 0,01 0,03 0,02 0,85 0,99 0,53
K2O 0,05 0,26 0,12 0,14 0,38

0,24

 0,01 0,01 0,01 0,27 0,15 0,25








 
 Dakhla Glass (Egypt) Type: ? Age: 28 -29 Ma (Oligocene)
The Dakhla glass is found also in the western desert in Egypt, nearby the oasis Dakhla. The Dakhla Glass (DG) is a volcanic glass (see). The high capacity of CaO and Al2O3 (18-25 wt%) points to a basaltic eruptiva. The Dakhla Glass (DG) has emerged at the same time like the Libyan Desert Glass. The distance of the localities the LDG and the DG is insignificant.
Both glasses differ however by the chemistry. The DG is volcanic or subvolcanic of origin, the LDG is sooner orthomagmatic-hydrovolcanic of origin.
The Dakhla Glass after transport and destruction was deposited in a new position. Now it is found as clumps in younger sediments.

Up to now are no exact chemical analyses known.



2. Tektite & Microtektite



 

 Tektites are a group of natural glasses occurring in at least four different strewn fields on earth. The largest strewn field includes Australia, Philippines, Indonesia, Vietnam, Thailand, Cambodia, Laos, Tibet and the southern China. Tektites are generally small, brownish to black, partly transparent, spherically symmetric, and sometimes aerodynamically ablated. Strewn fields are geographically restricted areas on earth where tektites are found, usually in association with microtektites.
Mikrotectites belonging to the Australasian, Ivory Coast, and North American tektite strewn fields have been found in marine sediments adjacent to the respective tektite strewn fields.
Australasian microtektites habe been recovered from approx. 50 cores taken in the Indian Ocean, western equatorial Pacific Ocean, and Philippine, Sulu, Celebes, and South China Seas. The Australasian microtektites are Middle Pleistocene in age.
North American microtektites have been found in Upper Eocene marine sediments on Barbados and in cores recovered from the Gulf of Mexico, Caribbean Sea, and north-western Atlantic Ocean (continental slope off New Jersey). The layers from Barbados indicates an age of ~35 Ma. The major oxide composition and age of the North American microtektites (and tektite fragments) suggest that they too belong to the North American tektite strewn field.
The Ivory Coast microtektites have been found in 11 cores in the eastern equatorial Atlantic Ocean. The layers is also Middle Pleistocene in age (~1.1 Ma). They have a restricted range in major element composition compared with the Australasian and North American microtektites.
 
 Moldavite (Europe)  Type: Rhyolitic Age: 14.4 - 15.1 Ma (Miocene)
The Moldavite are rhyolitic glasses. Their affinity to the supposed German impact structures  -- the Nördlinger Ries or the Steinheim basin -- is arbitrary. In the Bohemia and Moravia regions exist numerous Miocene volcanic structures, which come in consideration as source.
  
Oxide   (wt%) Bouska et al. (1973) etc. Bouska et al. (1973) etc. Bouska et al. (1995) Koeberl et al. (1988)
Moravia Bohemia Cheb Austria
range (21) average range (61) average range (4) average range (7) average
SiO2 74,90 81,40 78,15 75,50 85,10 80,30 78,46 79,89 78,97 78,10 85,10 79,73
Al2O3 9,44 13,80 11,62 7,32 11,40 9,36 8,38 10,13 9,17 8,10 10,60 9,81
TiO2 0,31 1,40 0,85 0,24 0,74 0,49 0,28 0,40 0,33 0,24 0,35 0,30
FeO 1,72 3,50 2,61 1,08 2,93 2,00 1,34 1,86 1,54 1,02 1,78 1,54
MgO 1,13 2,06 2,00 1,34 2,74 2,04 1,86 2,75 2,34 1,10 2,03 1,72
CaO 0,95 3,17 2,06 1,21 3,96 2,58 2,35 4,56 3,60 1,46 3,30 2,41
Na2O 0,40 1,08 0,74 0,20 0,89 0,54 0,31 0,59 0,41 0,19 0,49 0,39
K2O 2,83 3,81 3,32 2,23 3,81 3,02 2,61 3,85 3,24 2,62 3,90 3,49

 
Oxide   (wt%) Lange (1995)
Southern Bohemia Radomilice Western Moravia Lusatian area
range (43) average range (3) average range (46) average range (15) average
SiO2 71,90 81,00 78,60 80,00 84,70 82,60 74,91 83,10 79,28 77,2 84,10 79,30
Al2O3 8,96 12,70 10,10 7,27 9,36 8,22 9,27 13,18 11,01 8,94 11,80 10,50
TiO2 0,23 0,50 0,31 0,24 0,29 0,26 0,30 0,72 0,42 0,26 0,42 0,34
FeO 1,28 2,86 1,62 1,00 1,41 1,18 1,40 3,50 2,26 1,32 2,51 1,84
MgO 1,52 3,73 2,33 1,60 2,26 1,91 0,88 2,11 1,39 1,06 2,73 1,75
CaO 2,05 4,48 2,98 1,80 2,82 2,29 0,61 3,11 1,64 0,93 3,85 2,00
Na2O 0,25 0,60 0,42 0,19 0,32 0,24 0,27 1,08 0,57 0,28 0,70 0,47
K2O 2,88 3,77 3,40 2,20 2,97 2,53 2,60 3,81 3,38 3,06 3,75 3,46






 
 Indochinite (Indochina)  Type: Rhyolitic Age: 0.7 - 0.8 Ma (Pleistocene)
Indochinite are Fe-rich rhyolitic glasses. They are found far spreads in a region, in which since long time of the earth history volcanic activities intense presumably already ruled. The large strewn field includes Philippines, Indonesia, Vietnam, Thailand, Cambodia, Laos, Tibet and the southern China. Probable have thrown powerful volcanic explosions the glassy masses until on the Australian craton (Australite).
Within one strewn field, we can distinguish between splash-form tektites (normal tektites) and so called Muong Nong tektites, which differ from normal tektites in respect to a higher volatile content and greater inhomogeneity, besides being of generally larger size.
 
Oxide wt%) Son & Koeberl (2004) Chapman & Scheiber (1969) Koeberl (1992) Barnes & Pitakpaivan Lee et al.
Philippines (splash-type) Vietnam (MN-type) Philippinite MN-typ splash-typ Phang Daeng (Thailand) East Asia
range (6) average range (11) average range (12) average average (19) average (?) range (5) average average (30)
SiO2 71,63 73,21 72,62 74,92 78,14 77,05 67,20 74,90 70,62 78,93 72,70 72,44 80,40 75,42 74,36
Al2O3 11,69 12,04 11,87 10,07 12,20 11,08 8,90 17,70 13,20 10,18 13,37 9,50 13,34 11,72 11,13
TiO2 0,67 0,74 0,71 0,65 0,77 0,71 0,50 1,00 0,76 0,63 0,78 0,62 0,76 0,70 0,78
FeO 3,89 4,30 4,16 3,67 4,21 3,88 3,87 5,87 4,80 3,74 4,58 3,00 4,29 3,72 4,99
MgO 2,08 2,14 2,13 1,52 1,77 1,79 1,87 3,15 2,44 1,43 2,14 1,30 2,00 1,76 2,59
CaO 3,68 3,81 3,77 1,18 1,39 1,27 1,37 9,77 4,08 1,21 1,98 1,10 2,24 1,85 2,14
Na2O 1,09 1,22 1,66 1,04 1,20 1,09 0,91 1,50 1,19 0,92 1,05 1,20 1,62 1,48 1,43
K2O 2,32 2,44 2,39 2,35 2,53 2,46 1,77 2,81 2,34 2,42 2,62 2,20 2,48 2,35 2.39

 
Oxide wt%) Lee et al. (2003)
Wenchang
(China)		 Penglei
(China)		 Khon Kaen
(Thailand)		 Bao Loc
(Vietnam)		 Maoming
(China)		 Rizal
(Philippines)
range (5) average range (5) average range (5) average range (5) average range (5) average range (5) average
SiO2 72,12 72,69 72,49 71,84 74,49 73,06 72,18 74,07 73,25 72,26 73,61 72,93 77,26 80,61 78,53 75,10 76,95 75,87
Al2O3 12,88 14,32 13,73 12,47 14,61 13,54 13,19 14,47 13,75 12,35 12,81 12,61 5,15 8,46 7,06 5,35 6,99 6,07
TiO2 0,73 0,79 0,75 0,71 0,82 0,77 0,70 0,78 0,74 0,82 0,84 0,83 0,72 0,84 0,78 0,78 0,89 0,82
FeO 5,05 5,34 5,16 4,29 4,72 4,55 4,99 5,34 5,15 4,43 4,56 4,52 4,70 5,52 5,11 5,30 5,63 5,45
MgO 3,15 3,65 3,38 1,47 1,82 1,70 2,57 2,80 2,69 2,57 2,71 2,62 2,10 2,64 2,31 2,71 2,92 2,87
CaO 1,01 1,12 1,10 1,85 2,08 1,97 0,34 0,45 0,43 1,59 2,11 1,76 2,61 3,29 3,01 3,58 5,04 4,58
Na2O 1,33 1,45 1,40 1,40 1,63 1,53 1,33 1,48 1,40 1,24 1,35 1,32 1,18 1,43 1,30 1,57 1,76 1,62
K2O 2,14 2,34 2,30 2,53 2,65 2,61 1,98 2,26 2,15 2,38 2,53 2,45 2,12 2,38 2,27 2,44 2,68 2,54



Thailand



Section through an Indochinite



Vietnam



 



Thailand



China



Philippines

        
China                                                                                            China                                                                                           China



Philippines



Philippines
 Tibetanite (Tibet) Type: Rhyolitic Age: 0.7 - 0.8 Ma (Pleistocene)

The specimens from Tibet resembled typical Indochinites in superficial appearance and colour. The results of chemical analysis were essentially identical to Indochinites. By the K/Ar dating found to be 0,76 Ma, also consistent with the Australasian strewn field.



 
 Australite (Australia) Type: Rhyolitic Age: 0.7 - 0.8 Ma (Pleistocene)
The Australite like the Indochinite are Fe- rich rhyolitic glasses. Both types belong to the strewn-field "Australasian".
 
Oxide   (wt%) Australites
(Mason, 1979)		 Australites
(Taylor & Sachs, 1964)		 Australasian tektites
(Chapman & Scheiber, 1969)		 Australasian
 MN-type
(Glass & Koeberl, 1989)
range (60) average  range (15) average range (51) average range (8) average average (?)
SiO2 67,30 78,90  73,06 69,67 77,39 73,53 64,76 82,40 73,58 67,40 73,15 70,28 72,50
Al2O3 9,50 15,90 12,23  9,84 13,96 11,90 8,20 17,70 12,95 10,90 12,90 11,90 12,94
TiO2 0,59 0,85 0,68 0,60 0,90 0,75 0,43 1,00  0,72 0,64 0,76 0,70 0,76
FeO 3,55 6,10 4,14  3,84 5,48 4,66 3,09 8,63 5,86  5,65 7,82 6,74 4,76
MgO 1,31 3,53 2,04 1,60 2,89 2,24 1,13 7,95 4,54  3,48 6,38 4,93 2,08
CaO 1,57 5,93 3,38 2,39 4,77 3,58 0,73 9,77 5,25  2,10 3,47 2,78 2,49
Na2O 0,91 1,74 1,27  1,05 1,50 1,28 0,62 1,70 1,16 0,62 1,22 0,92 1,42
K2O 2,08 2,78 2,20  2,07 2,57 2,32 1,34 2,81 2,08  1,44 2,23 1,84 2,64

 

Oxide   (wt%) Australites  (Chapman & Scheiber, 1969) Australites (Taylor &Sachs, 1964)

Australasian Microtektites (Glass et al., 2003)
range (11) average  range (23) average range (32) average range (30) average  range (7) average
SiO2 66,90 79,70 71,13 66,90  79,70 73,30 69,60 78,70 74,15 60,48 78,05 69,60 66,69 72,01 69,35
Al2O3  9,30  16,10 13,72 9,90  16,10 13,00 9,35 14,00 11,68 10,25 21,46 14,90 12,48 14,94 13,54
TiO2 0,49 0,93 0,79 0,48 0,93 0,70 0,55 0,90 0,72 0,64 1,18 0,82 0,69 0,81 0,75
FeO 3,57 5,43 4,78 3,57 6,06 4,82 3,83 5,38 4,60 2,90 6,32 5,08 5,11 6,77 5,96
MgO 1,31 2,60 2,21 1,31 4,28 2,80 1,49 2,49 1,99 1,67 5,07 3,23 2,90 4,17 3,41
CaO 1,83 5,48 3,45 1,72 5,62 3,67 2,13 5,09 3,61 1,63 6,56 3,52 2,37 4,30 3,06
Na2O 1,00 1,56 1,24 1,00 1,58 1,29 1,05 1,52 1,28 0,28 1,70 0,92 0,98 1,59 1,30
K2O 2,14 2,62 2,39 2,00 2,62 2,31 2,07 2,57 2,32 0,67 2,86 1,83 2,22 2,86 2,57



Flying drops



 

 Ivorite (Ivori Coast) Type: Dacitic Age: 1.1 Ma (Pleistocene)
The rare Ivorite in their chemistry are not absolutely comparable to the Indochinite and Americanite. They are Fe-rich dacitic glasses. The blisters-structure is remarkable, which is comparable with the volcanic Obsidian. As source is supposed the crater Bosumtwi in Ghana. The crater would be then no impact structure, but an explosive volcanic structure.
  
Oxide
(wt%)		 King, 1976 Chapman & Scheiber
(1969) etc.		 Koeberl et al. (1997) Microtektites
Glass et al., 2003 Koeberl et al., 1998
average (?) range (15) average average (11) range (16) average average (4)
SiO2 71,05 67,00 69,30 68,15 67,58 63,32 69,30 66,38 67,40
Al2O3 14,60 15,80 17,10 16,45 16,74 15,82 17,62 16,86 17,10
TiO2 0,70 0,52 0,60 0,56 0,56 0,47 0,62 0,55 0,59
FeO 5,51 6,03 6,80 6,42 6,16 6,12 7,49 6,65 6,40
MgO 3,27 2,64 3,93 3,28 3,46 2,91 6,30 4,27 3,70
CaO 1,67 0,71 1,61 1,16 1,38 1,05 2,34 1,73 1,22
Na2O 1,71 1,54 2,44 1,99 1,90 1,60 2,19 1,92 1,63
K2O 1,53 1,70 2,07 1,88 1,95 1,00 2,03 1,60 1,86



 



 
 Americanite (USA)  Type: Rhyolitic Age: 34.5 - 35.5 Ma (Eocene)
Tektites belonging to the North American strewn field are found in Texas (Bediasites), and found in Georgia (Georgianites). One tektite found in Massachusetts (Martha's Vineyard). They are found in Eocene sediments. Microglasses are found in marine sediments nearby the coast and in the Caribbian Sea. They all would be with it clearly the oldest glasses. There is a great amount of chemical analyses. The chemistry of both - the Caribbean glasses as well as the Bediasite and Georgianite - is identical. The Americanite like the younger Australasian are rhyolitic glasses. As source is supposed a large crater-shaped structure, which is located in the Chesapeak Bay at the coast of Virginia.
 

Oxide
(wt%)

Georgianites

Bediasites

Martha's Vineyard

 Cuba
Albin et al. (2000)

Cuttitta et al. (1967)

 Wittke & Barnes Chao (1963)

average (24)

range (9)

average

range (25)

average (35)

range (21)

 average (21) single single

SiO2

81,80

79,80

83,60

81,50

71,89

81,31

76,36

71,90

 80,20

76,37

 80.50 74,80

Al2O3

11,20

9,50

11,7

10,71

10,96

17,56

13,77

11,20

 17,60

13,78

 11,20 15,00

TiO2

0,51

0,42

0,60

0,49

0,53

1,05

0,77

0,59

 1,05

0,76

 0,53 0,80

FeO

2,64

1,83

3,14

2,50

2,29

5,95

4,01

2,29

 5,75

3,98

 2,69 4.40

MgO

0,61

0,37

0,69

0,55

0,37

0,95

0,69

0,37

 0,95

0,63

 0,69 0,70

CaO

0,45

0,40

0,69

0,51

0,41

0,96

0,56

0,49

 0,96

0,65

 0,69 1,20

Na2O

2,44

1,00

1,53

1,19

1,20

1,84

1,51

1,20

 1,84

1,54

 1,00 1,10

K2O

0,94

2,22

2,51

2,39

1,60

2,43

2,04

1,60

 2,43

2,08

 2,37 2,00

 

Oxide
(wt%)

 Microtektites, NA Mikrotektites

Tektite Barbados

 Microtektites Barbados
Wittke & Barnes Glass et al.

Koeberl & Glass (1987)

 Glass et al. (2003)

Koeberl & Glass (1987)
range (55) average (25) single single single aver. (9) aver. (27) single single single range (18)

SiO2

 63,52 84,16 73,4

79,50

79,10

77,40

 80,40 76,10

77,40

79,50

82,00

 76,90 85,60

Al2O3

 8,15 17,75 14,10

12,50

12,10

12,90

 11,30 12,4

13,50

12,10

10,30

 7,97 14,80

TiO2

 0,30 1,08 0,73

0,62

0,43

0,69

 0,56 0,55

0,71

0,59

0,41

 0,40 0,71

FeO

 2,06 6,24 4,37

2,35

2,42

3,02

 2,75  4,27

3,98

3,45

2,48

 1,37 3,98

MgO

 0,00 3,26 1,73

0,74

0,92

0,80

 0,46 1,08

0,64

0,58

0,48

 0,13 1,13

CaO

 0,27 2,97 1,64

0,19

0,74

0,75

 0,68 1,12

0,59

0,57

0,65

 0,52 0,87

Na2O

 0,17 3,04 1,06

1,17

1,24

1,23

 1,27  1,18

1,26

1,29

1,23

 1,15 1,52

K2O

 1,91 4,03 2,92

2,49

2,71

2,73

 2,25 2,69

1,94

1,93

2,42

 1,73 2,54

 
Oxide
(wt%)

Tektite, DSDP 612

Mikrotektite, DSDP 612

 Microtektites DSDP 612

 Microtektites DSDP 904

 Microtektites RC9-58

Koeberl & Glass (1987)

 Glass et al. (2003)

 Glass et al. (2003)

 Glass et al. (2003)
single single single single single single range (8) average (23) average (28) range (11) average
SiO2

72,30

74,20

77,60

71,36

73,37

75,28

 71,90 77,80 72,30