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Sills greater 150m can place country rocks into the oil and gas window out to ~4km. • Evidence for magmatic thermal pertubation other than burial, can be seen in thermal maturity data.

New developments in in-situ dating of shales: Rb–Sr via LA–QQQ–ICP–MS ARC Mc Arthur Basin Linkage Team (1) Introduction: 87 87 The Rb–Sr dating technique, based on the radiactive decay of Rb to Sr, is a well established technique.

160 a) 50m sill 150 140 140 130 130 120 110 100 110 100 90 80 80 70 70 60 1500 2000 2500 3000 Distance from sill wall (m) 3500 4000 4500 60 5000 1500 160 160 150 140 130 130 120 120 110 90 80 80 r yr ky 10 r 1000 7k 5ky 500 2kyr 1kyr 0.8kyr 0.5kyr 0.1kyr 0.3kyr 0.01kyr 0 1500 ky r 20 ky r 30 ky 2000 r 50k yr 2500 100kyr 3000 Distance from sill wall (m) 15 10 50 70 15 m 0m sil l 200kyr 3500 4000 4500 5000 4000 4500 5000 100 90 70 Distance from sill wall (m) 3500 as 100 3000 &G 110 2500 Oil Temperature (C) 140 2000 d) Time integrated thermal effect Gas c) 150m sill 150 Temperature (C) 120 90 60 b) 100m sill 150 Temperature (C) Temperature (C) 160 60 0m sill sill 15 2500 3000 Distance from sill wall (m) 3500 4000 4500 5000 Figure 3. Also shown is the location of a Derim Derim sill, thickness of this sill is unknown. This is consistent with the intrustion of the magmatic sills. 1313 Ma mafic magmatism is geographically widespread in the NT.

Thermal models showing the extent of country rock heating associated with emplacement of doleritic sills of various thicknesses. Two defined Tmax (ºC) gradients can be observed in Altree 2. Model parameters: Limitations: • 1250 ºC emplacement tem• Static burial history. • Instantaneous and non-con• 50ºC background tempera- tinuous sill emplacement. • Emplacement temperatures of up to ~1250ºC are characteristic of both the sills and dykes.

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Become part of the new community at SHARE Your Dating Stories – a new social media platform where you can interact with other members in exchanging stories, ideas, advice and experiences about dating.Practical considerations means that the number of analyses that are used to define an isochron is limited.