by rockdoc123 » Fri 30 Nov 2012, 11:11:54
$this->bbcode_second_pass_quote('', 'S')o that sounds like the Mackenzie Delta in Canada and the Ob, Lena and Enisei in Siberia. Does the river have to be one of the big four to make the kind of delta you are referring too or will smaller rivers do the same thing just at a slower rate of deposition?
the main components in the equation that describes source rock maturation and expulsion is temperature and time and type of source rock. The activation energy associated without different kerogen types governs the rate at which a particular source rock expels hydrocarbons. As a consequence Type I kerogens might have to be buried deeper to get the same maturity as their Type II conterparts. Temperature is by far the more important to the extent that some authors have argued that it is strictly a temperature relationship although that isn't mainstream thinking. Temperature has several components that are important, firstly the crustal type governs largely what heat flow recognized in the sedimentary column will be. Continental crust is thick and heat flows are much lower than oceanic crust which is thin, transitional crust being in the middle. As well the type of sediment deposited has some influence as different rock types have different thermal characteristics. Time refers to how long a particular source rock remains buried at elevated temperatures. In deltas the deposition is quite quick so there is a chance to get younger source rocks mature quicker. Unfortunately there is no rule of thumb as to burial depth. My guess (and I qualify that as being a wild ass guess) without having any data is that you probably need burial depths of 2.5 to 4.0 km before you would see much in the way of oil generation unless, of course, the heat flow is higher than I am assuming (I am guessing it is somewhere around 40 - 60 mW/m2).
You might want to check the USGS website. As I remember about 3 or 4 years ago they did an Arctic Ocean analysis of future hydrocarbon potential and put together a map that highlighted the areas with greatest potential. As I recall it seemed to be mainly gas prone but can't remember exactly.