<h3 style="margin-top:auto;margin-left:auto;margin-right:auto"><span class="mw-headline"><span style="font-weight:normal;font-size:12pt;font-family:Verdana">Hi andrew, here are some forms or organics and </span></span><span style="font-weight:normal;font-size:12pt;font-family:Verdana">kerogen to look for coming out of those ovens- there are four types, I just gave two of the most interesting.</span></h3><h3 style="margin-top:auto;margin-left:auto;margin-right:auto"><span class="mw-headline"><span style="font-weight:normal;font-size:12pt;font-family:Verdana">Type I</span></span></h3><ul><li class="MsoNormal" style="margin-top:0in;margin-left:0in;margin-right:0in;tab-stops:list.5in"><span style="font-family:Verdana">containing
alginite, amorphous organic matter,
cyanobacteria,
freshwater algae, and land plant
resins (AMO) </span></li><li class="MsoNormal" style="margin-top:0in;margin-left:0in;margin-right:0in;tab-stops:list.5in"><span style="font-family:Verdana">
Hydrogen:
Carbon ratio > 1.25 </span></li><li class="MsoNormal" style="margin-top:0in;margin-left:0in;margin-right:0in;tab-stops:list.5in"><span style="font-family:Verdana">
Oxygen:Carbon ratio < 0.15 </span></li><li class="MsoNormal" style="margin-top:0in;margin-left:0in;margin-right:0in;tab-stops:list.5in"><span style="font-family:Verdana">Shows great tendency to readily produce
liquid hydrocarbons. </span></li><li class="MsoNormal" style="margin-top:0in;margin-left:0in;margin-right:0in;tab-stops:list.5in"><span style="font-family:Verdana">It derives principally from
lacustrine algae and forms only in
anoxic lakes and several other unusual marine environments </span></li><li class="MsoNormal" style="margin-top:0in;margin-left:0in;margin-right:0in;tab-stops:list.5in"><span style="font-family:Verdana">Has few
cyclic or
aromatic structures </span></li><li class="MsoNormal" style="margin-top:0in;margin-left:0in;margin-right:0in;tab-stops:list.5in"><span style="font-family:Verdana">Formed mainly from
proteins and
lipids </span></li></ul><h3 style="margin-top:auto;margin-left:auto;margin-right:auto"><span style="font-weight:normal;font-size:12pt;font-family:Verdana"><span class="mw-headline">Type II</span></span></h3><ul><li class="MsoNormal" style="margin-top:0in;margin-left:0in;margin-right:0in;tab-stops:list.5in"><span style="font-family:Verdana">Hydrogen:Carbon ratio < 1.25 </span></li><li class="MsoNormal" style="margin-top:0in;margin-left:0in;margin-right:0in;tab-stops:list.5in"><span style="font-family:Verdana">Oxygen:Carbon ratio 0.03 to 0.18 </span></li><li class="MsoNormal" style="margin-top:0in;margin-left:0in;margin-right:0in;tab-stops:list.5in"><span style="font-family:Verdana">Tend to produce a mix of gas and oil. </span></li><li class="MsoNormal" style="margin-top:0in;margin-left:0in;margin-right:0in;tab-stops:list.5in"><span style="font-family:Verdana">Several types:
exinite,
<span style="color:#cc2200">cutinite</span>,
<span style="color:#cc2200">resinite</span>, and
<span style="color:#cc2200">liptinite</span> </span><ul><li class="MsoNormal" style="margin-top:0in;margin-left:0in;margin-right:0in;tab-stops:list1.0in"><span style="font-family:Verdana">
Exinite: formed from the casings of
pollen and
spores </span></li><li class="MsoNormal" style="margin-top:0in;margin-left:0in;margin-right:0in;tab-stops:list1.0in"><span style="font-family:Verdana">
<span style="color:#cc2200">Cutinite</span>: formed from terrestrial
plant cuticle </span></li><li class="MsoNormal" style="margin-top:0in;margin-left:0in;margin-right:0in;tab-stops:list1.0in"><span style="font-family:Verdana">
<span style="color:#cc2200">Resinite</span>: formed from terrestrial plant resins and animal decomposition resins </span></li><li class="MsoNormal" style="margin-top:0in;margin-left:0in;margin-right:0in;tab-stops:list1.0in"><span style="font-family:Verdana">
<span style="color:#cc2200">Liptinite</span>: formed from terrestrial plant
lipids (
hydrophobic molecules that are soluble in organic solvents) and marine algae </span></li></ul></li></ul><p><span style="font-family:Verdana">They all have great tendencies to produce petroleum and are all formed from lipids deposited under
reducing conditions.</span></p><p><span style="font-family:Verdana">
<font color="#800080">http://en.wikipedia.org/wiki/Kerogens</font></span></p><p><span style="font-family:Verdana">
<span style="color:#cc2200"><font color="#000000">Van Krevelen diagram</font></span></span></p><p><span style="font-family:Verdana">
<font color="#800080">http://userpage.fu-berlin.de/~cheubeck/classes/Petroleumgeologie/class_content/03_Geochem_bw.pdf</font></span></p><span style="font-family:Verdana"><p><span style="font-size:12pt;font-family:Verdana">My favorite - Type 1 and finding methane</span></p></span> <div class="Discussion_UserSignature"> Ron Bennett </div>