If you consider it as a continental-scale process with a rift system like the EARS consisting of many branches, some of them developing into failed rifts, the process probably can take longer than 60 million years. See e.g. the Jurassic to Cretaceous rift basins of Sudan - if today's rift systems in East Africa have formed in continuation of certain (failed) Mesozoic rifts you would have a continenctal-scale process lasting more than twice as long. How long it takes from the intial phase to oceanic crust formation probably depends on various facors, such as rate of divergence, thickness, compositon/age of the continental crust subjected to rifting.
You are rigth, but I am more interested in the continental-rift to oceanic crust formation case. Is there any well-studied example lasting several tens of m.y.?
Papers by Luyendyk and his team and no doubt others document that the part of the West Antarctic rift system through Marie Byrd Land started extending about104 Ma, and then New Zealand/Campbell Plateau started drifting away about 80 Ma. But the rifting continued in Ross Sea, with possible early Cenozoic rifting in the middle of Ross Sea and definite Eocene-Oligocene large rifting in Western Ross Sea opposite Adare Trough spreading. And the Terror Rift is still active.
For Continent to Ocean, you might want to look at the north Atlantic: the rifts in eastern USA. But I don't know the timing.
probably the best studied continental margin is the Newfoundland - Iberia conjugate system. There is a wealth of data coming from the ODP and DSPD projects. You should consider having a look at their summaries. These scientific missions have drilled several sites at both margins, as well as acquired many km of seismic profiles. Actually, most of the existing models for rifting and oceanic spreading come from the data obtained for this conjugate system. More indirect evidence comes from the study of 'well' preserved ocenanic remmants in orogenic belts such as the Alps, Dinarides, Oman, Alaska, ...
You could consider having a look to the models made by Gianreto Manatschal and co-workers. They have a large data set mainly coming from Central Alps of Switzerland and Italy. In their works they present isotopic and biostratigraphy ages to constrain the timing of rifting and oceanic spreading. Whether you agree or not with their models it's fine, but they manage a large data set on timing. Another interesting indirect source of information comes from the Western Alps. A nice review is presented in the book "The Western Alps, from rift to passive margin to orogenic belt" by Pierre-Charles de Graciansky, Dave G. Roberts and Pierre Tricart". I am currently working the Eastern Alps, but I anyway find this text very very illustrative and it contains a fantastic compilation of many many years of work as well as constrasting views.
Going back to your question, rifting to oceanic spreading can last for many tens of Myrs. It depends on the case, but regarding the Pyrenean Rift - Bay of Biscay, final rifting episode started at about Kimmeridgian times (ca.155 Ma) and mantle exhumation - oceanic spreading halted by Santonian(?) times moreless (ca. 84 Ma). So for this case, yes. Consider also, as mentioned above by E. Lunding, that rifting of the Variscan edifice actually started by Permian - Triassic (Pangea break up), stopped during Early-Middle Jurassic and was resumed in Late Jurassic. So the whole process of rifting and spreading can last for way more than 60 Myr.
Another idea to find time constraints for the transition from continental rift to sea floor, especially a minimum duration, is to study very young rift basins and oceans. A good example might be the Afar triple junction where the Red Sea, Gulf of Aden, and northern part of the (Main) Ethiopian Rift join.
See e.g. the paper of Bosworth and colleagues (2005) on the timing of Red Sea and Gulf of Aden rifts: Accordling to the volcanic history (and further geological evidence) the phase of continental rifting (syn-rift phase) started during the Oligocene and ended during the Miocene. It took between 10 million years (Gulf of Aden and Gulf of Suez) and 22 million years (southern Red Sea).
Thanks for your help. I am reading some papers about the Afar triple junction. I have started with the 2006 Special Publication of the Geol Soc London (Yirgu et al.). Maybe there is something esle out there from other old rift systems.
Pablo, I will look up for the differences between magma-assisted and magma poor rifts, thanks!
The oldest volcanic rocks in relation to the onset of extension along the future Izmir-Ankara branch of Neotethys are late Ladianian in age Tekin U.K. & Goncuoglu,M.C. 2007. Discovery of oldest (late Ladinian to middle Carnian) radiolarian assemblages from the Bornova Flysch Zone in western Turkey: Implications for theevolution of the Neotethyan Izmir-Ankara Ocean. Ofioliti, 32/2, 131-150) The oldest oceanic pillow-lavas within the Izmir-Ankara suture belt are late Carnian in age (Tekin U.K., Göncüoglu M.C. and Turhan N., 2002. First evidence of Late Carnian radiolarians from the Izmir-Ankara Suture Complex, central Sakarya, Turkey: implications for the opening age of the Izmir-Ankara branch of Neo-Tethys. Geobios, 35/1, 127-135).
Accordingly, the time-span you are asking is about 10-12 Ma for the Izmir-Ankara Ocean. However, pleace notice that there are numerous controls and the data in literature is case-specific.
For an ancient example, during Neoproterozoic break-up of Rodinia, the eastern (present-day coordinates) margin of Laurentia experienced an ~200 m.y. history of rifting that occurred in two major pulses. The first episode, over the period of ca. 765-680 Ma, involved intracontinental rifting characterized by bimodal volcanism and intrusion of A-type granitoid plutons. There appears to have been a hiatus in activity until extrusion of basalt and minor rhyolite at ca. 570-555 Ma, during relatively rapid extension that led to continental break-up and opening of the Iapetus Ocean. A few pertinent references are: Aleinikoff et al., 1995, American Journal of Science, v.295, p.428-454; Fetter & Goldberg, 1995, Journal of Geology v.103, p.313-326; Tollo et al., 2004, Precambrian Research, v.128, p.3-38; Badger & Sinha, 2004, Geol Soc America Memoir 197, p.435-458.
Maybe you can have a look at the review paper by Ziegler and Cloetingh (Earth Science Reviews, 64, 1-50, 2004). The duration of rifting is highly variabile and they provide a quite long list of different examples in both volcanic and non-volcanic settings.
The expanding earth hypothesis is simply not true. I've addressed parts of this before to Clarke posts so will not bother here. I'm only posting in case some of the scientists reading this do not have much earth science background.
This reminds me of a thread on ResearchGate about whether dark energy has anything to do with plate tectonics. There are several what appear to be high-quality answers (answers are "No") and then a couple by a Russian scientist with a high RG score, higher than many serious scientists (including me). She with others self publishes on Research Gate that dark energy triggers earthquakes that in turn trigger giant whirlpools that sucked in Malaysian Flight 370. Some of her references were to fiction by Edgar Allen Poe, and there is some discussion of the Bermuda triangle having giant whirlpools (that said, there is a massive amount of methane hydrate on Blake Ridge and elsewhere which is within the so called Bermuda triangle, and I wonder if it is possible to have a large enough release to affect the surface: would probably have to be a release from a submarine slide).
I think this "scientist" has a RG score of about 33. RG is going to have to rethink the way they give "credibility". I never joined Facebook or any other social media until I joined RG, which I joined a few months ago because it was suggested for a promotion. So, I long though things like how many "friends" were kind of sad, although I'm impressed with Shakira's 70 or 90 million.
If anyone beside Michael need me to post a few major flaws in expanding earth, let me know and I will do so again. One could start with basic physics. Then, age of earth. Then, well-documented subduction and earthquakes. Then, GPS velocities.