GEOCAMP Institute
GEOCAMP Institute
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วีดีโอ

Reservoir Architecture, Correlation and Connectivity
มุมมอง 1519 ชั่วโมงที่ผ่านมา
Reservoir Architecture, Correlation and Connectivity
How Alluvial Deposits can become Hydrocarbon rich Reservoirs
มุมมอง 4619 ชั่วโมงที่ผ่านมา
How Alluvial Deposits can become Hydrocarbon rich Reservoirs
Alluvial Fans vs Basin Floor Fans Pt2 - Comparison
มุมมอง 1819 ชั่วโมงที่ผ่านมา
Alluvial Fans vs Basin Floor Fans Pt2 - Comparison
Alluvial Fans vs Basin Floor Fans Pt1 - Comparison
มุมมอง 1219 ชั่วโมงที่ผ่านมา
Alluvial Fans vs Basin Floor Fans Pt1 - Comparison
Erosional vs Depositional Fills from Strata Terminations - 2
มุมมอง 4319 ชั่วโมงที่ผ่านมา
Erosional vs Depositional Fills from Strata Terminations - 2
Sedimentary Facies Changes - Outcrop to Model scale
มุมมอง 4019 ชั่วโมงที่ผ่านมา
Sedimentary Facies Changes - Outcrop to Model scale
Sedimentary Facies and Reservoir Quality
มุมมอง 4319 ชั่วโมงที่ผ่านมา
Sedimentary Facies and Reservoir Quality
Erosional vs Depositional Fills from Strata Terminations - 1
มุมมอง 5119 ชั่วโมงที่ผ่านมา
Erosional vs Depositional Fills from Strata Terminations - 1
Delineating Boundaries using Facies Type and Strat Terminations- Pt2
มุมมอง 5019 ชั่วโมงที่ผ่านมา
Delineating Boundaries using Facies Type and Strat Terminations- Pt2
Delineating Stratal Boundaries using Facies Type and Strat Terminations Boundaries Pt1
มุมมอง 13019 ชั่วโมงที่ผ่านมา
Delineating Stratal Boundaries using Facies Type and Strat Terminations Boundaries Pt1
Fluvial Deposits - Traction Saltation Suspension
มุมมอง 144ปีที่แล้ว
An introduction to traction, saltation and suspension deposits in fluvial settings.
Fluvial Processes and Deposition Ripples
มุมมอง 154ปีที่แล้ว
A refresher on fluvial processes, current ripples and associated deposits and sedimentary structures.
Snippets- Nurturing Talents
มุมมอง 35ปีที่แล้ว
Snippets from a talk on growing or mentoring young talented individuals
Early Start (Tips) for Students_Geoscience Field and Laboratory Studies
มุมมอง 68ปีที่แล้ว
Shared a personal experience with some geoscience students and young professionals. Focus is on combating the phobia for field / laboratory studies, growing personal network and technical skills. Key message is 'Start Early' Target audience: Entry level undergraduate students.
ResGeo_13: Quick calculation and concluding thoughts
มุมมอง 48ปีที่แล้ว
ResGeo_13: Quick calculation and concluding thoughts
ResGeo_12: Reservoir Connectivity and Compartmentalization (Macroscale)
มุมมอง 84ปีที่แล้ว
ResGeo_12: Reservoir Connectivity and Compartmentalization (Macroscale)
ResGeo_11: Reservoir Connectivity and Compartmentalization (Megascale)
มุมมอง 165ปีที่แล้ว
ResGeo_11: Reservoir Connectivity and Compartmentalization (Megascale)
ResGeo_10: Hydrocarbon Fluid Distribution in Reservoir Rocks - Key Controls
มุมมอง 103ปีที่แล้ว
ResGeo_10: Hydrocarbon Fluid Distribution in Reservoir Rocks - Key Controls
ResGeo_09: Quartz Overgrowths and Pressure Solutions in Sandstone Petrographic Sections
มุมมอง 116ปีที่แล้ว
ResGeo_09: Quartz Overgrowths and Pressure Solutions in Sandstone Petrographic Sections
ResGeo_08: The Reservoir Rock Cycle - from Initial to Altered State
มุมมอง 38ปีที่แล้ว
ResGeo_08: The Reservoir Rock Cycle - from Initial to Altered State
ResGeo_07: Deformed or Stressed Reservoir Rocks - the Altered Product
มุมมอง 45ปีที่แล้ว
ResGeo_07: Deformed or Stressed Reservoir Rocks - the Altered Product
ResGeo_06: Reservoir Journey 3 (Response to Sedimentary Processes)
มุมมอง 51ปีที่แล้ว
ResGeo_06: Reservoir Journey 3 (Response to Sedimentary Processes)
ResGeo_05: Reservoir Journey 2 (Response to Basin Loading and Burial)
มุมมอง 59ปีที่แล้ว
ResGeo_05: Reservoir Journey 2 (Response to Basin Loading and Burial)
ResGeo_04: Reservoir Journey 1 (Rock Response to Tectonics)
มุมมอง 66ปีที่แล้ว
ResGeo_04: Reservoir Journey 1 (Rock Response to Tectonics)
ResGeo_03: The Reservoir at Initial Conditions
มุมมอง 70ปีที่แล้ว
ResGeo_03: The Reservoir at Initial Conditions
ResGeo_02: Surface and Subsurface Reservoir Occurrences - Outcrops, Well Cores, Wireline Logs
มุมมอง 101ปีที่แล้ว
ResGeo_02: Surface and Subsurface Reservoir Occurrences - Outcrops, Well Cores, Wireline Logs
ResGeo_01: What is a Reservoir Rock?
มุมมอง 131ปีที่แล้ว
ResGeo_01: What is a Reservoir Rock?
Integrated clip MakerereJune18 20221
มุมมอง 422 ปีที่แล้ว
Integrated clip MakerereJune18 20221
4b_Channel fills Levees and Exploration well placements
มุมมอง 842 ปีที่แล้ว
4b_Channel fills Levees and Exploration well placements

ความคิดเห็น

  • @abu-zulaikhastudio
    @abu-zulaikhastudio 8 วันที่ผ่านมา

    Educative❤

  • @abu-zulaikhastudio
    @abu-zulaikhastudio 8 วันที่ผ่านมา

    Great work Sir ❤

  • @IlluminateYourMind247
    @IlluminateYourMind247 8 วันที่ผ่านมา

    Hello, Dr. Obi. I went on a field trip last year, and for the first time, I saw and heard of "Shale/mud-filled channels". They were described as channels that were originally filled with sand but got eroded and filled up with mud/shaly materials from episodes of deposition when things were a lot calmer. Is that a possibility here? Because I hear you describe the contents in this channel feature containing sufficient mud materials. Thank you.

    • @GEOCAMPInstitute_iso
      @GEOCAMPInstitute_iso 7 วันที่ผ่านมา

      @@IlluminateYourMind247 Very possible. Sometimes the current fill you see is not the initial item that filled the channel. It could be the second or third phase materials that eventually get preserved in the channel which.

  • @alabipaul9835
    @alabipaul9835 8 วันที่ผ่านมา

    Thanks for sharing Dr. Obi

  • @JeremyWeston-l7o
    @JeremyWeston-l7o หลายเดือนก่อน

    Currently looking at a similar system in the Gulf of Mexico for my masters, no one does a good job at explaining some of their terms used in their papers because it’s for a field for experts so as a geophysicist trying to put together my geologic background I thank you!

  • @sarfealam2414
    @sarfealam2414 8 หลายเดือนก่อน

    Thank you ❤

  • @anyajianita
    @anyajianita 10 หลายเดือนก่อน

    Thank you for this! it was really helpful.

  • @abu-zulaikhastudio
    @abu-zulaikhastudio 10 หลายเดือนก่อน

    Great 👍

  • @wwlittle
    @wwlittle ปีที่แล้ว

    I have enjoyed your series. Good, clear explanations and illustrations. I do have one concern with this video. It appears that you might not be taking into account surface topography and parallax with respect to systems tracts on your photo. In particular, the upper "sequence boundary" seems to simply reflect the modern erosional surface, rather than a real stratigraphic feature. While it does illustrate the concept well, I think that is a bit misleading.

  • @usmanmustapha1768
    @usmanmustapha1768 ปีที่แล้ว

    Horizontally

  • @nojiratzlaff4388
    @nojiratzlaff4388 ปีที่แล้ว

    You never explain why there are two high tides each day. While the moon is pulling on one side of the Earth, creating high tide there, what's pulling on the other side, creating high tide there?

  • @balachandargovindan3426
    @balachandargovindan3426 ปีที่แล้ว

    you teaching simply and understanding manner . After seeing you lecture, lot of my doubt is cleared . Thank you very much sir. Love from India🙏

  • @tuberider1171
    @tuberider1171 ปีที่แล้ว

    Can anyone explain whether the Spring tide ranges vary depending on whether the moon is closest to the sun or on the other side of the earth. That is, is the Spring tide greater when the moon is closest to the sun rather than on the far side of earth? I was wondering if the combined gravitational force of both the sun and the moon would cause a greater tidal range than when the moon was on the opposite side of the earth. I could look up charts I guess but was curious as to whether there was a video explaining this somewhere.

  • @TheBtrivedi
    @TheBtrivedi 2 ปีที่แล้ว

    Thank you. Would be great to include the cross section of channel 1, 2, 3, 4, 5 on the main slide too (helps a lot to non geologists like me), this is especially as you said one has to think in 3D.

    • @GEOCAMPInstitute_iso
      @GEOCAMPInstitute_iso 2 ปีที่แล้ว

      Great suggestion! Will keep that in mind when doing a follow up. Thanks!

  • @TheBtrivedi
    @TheBtrivedi 2 ปีที่แล้ว

    Thank you, great video.

  • @ibrahimemad6534
    @ibrahimemad6534 2 ปีที่แล้ว

    thanks, GEOCAMP, very interesting

  • @stephenyebaoh956
    @stephenyebaoh956 2 ปีที่แล้ว

    rivers and stream flow from its tributary on their pathway from natural landscape , the faster flowing of water sources cause erosion that is , the basin drainage carrying sediment from the mouth of upper stage and continue carrying in the channel pathway in the middle stage to create new habitat for some organism in their system erosion and deposition to the lower stage that's deposition to drop off the carrying sediment and pebbles in the deeper sea or the ocean

  • @mawukofianyo5345
    @mawukofianyo5345 2 ปีที่แล้ว

    Great. Easy to understand these paloeacurrent structures in your video.

  • @ilyestabti5757
    @ilyestabti5757 2 ปีที่แล้ว

    thank you sir

  • @oghenerosiloko9203
    @oghenerosiloko9203 2 ปีที่แล้ว

    Currently learning this at centre of excellence...and this video just cemented my understanding

  • @mikalkahsay8133
    @mikalkahsay8133 3 ปีที่แล้ว

    Nicely explained

  • @bossunable
    @bossunable 3 ปีที่แล้ว

    thanks, this was absolutely briliant.

  • @rappar9673
    @rappar9673 3 ปีที่แล้ว

    Nice videos sir.

  • @fieldsolutionsHub
    @fieldsolutionsHub 3 ปีที่แล้ว

    Wow. These descriptions are eductive.

  • @ronalddaviddada5846
    @ronalddaviddada5846 3 ปีที่แล้ว

    Good stuff Obi.. Actually learnt something new.

  • @nayanchoudhary9629
    @nayanchoudhary9629 3 ปีที่แล้ว

    Fault propagation fold generated by which thrust?

  • @alexnoskov1206
    @alexnoskov1206 3 ปีที่แล้ว

    Hi! So... correlative conformity in well section could be represented by limestones (shallow marine sedimentation)?

  • @AbhishekKumar-ry9ls
    @AbhishekKumar-ry9ls 3 ปีที่แล้ว

    Nice🤩 in depth explanation

  • @AbhishekKumar-ry9ls
    @AbhishekKumar-ry9ls 3 ปีที่แล้ว

    Well explained ❤️

  • @geologist933
    @geologist933 3 ปีที่แล้ว

    Thanks Could you make well log correlation video?

  • @zakriyaalsubhi1322
    @zakriyaalsubhi1322 3 ปีที่แล้ว

    Great and simple presentation. Thanks

  • @Therealutanmen
    @Therealutanmen 3 ปีที่แล้ว

    thank you!!!

  • @maryjaneconstancio6870
    @maryjaneconstancio6870 3 ปีที่แล้ว

    Where's the link pls i need to sent it to my online class

  • @ScentBlast
    @ScentBlast 3 ปีที่แล้ว

    Outstanding video. Helped a lot. Thank you.

  • @impressionk3938
    @impressionk3938 4 ปีที่แล้ว

    How can we find the channel from logs other than GR logs?

  • @marwanelsayed2282
    @marwanelsayed2282 4 ปีที่แล้ว

    it did worth my while thanks

  • @marwanelsayed2282
    @marwanelsayed2282 4 ปีที่แล้ว

    i wanna say you are a life saver

  • @verchassingh9277
    @verchassingh9277 4 ปีที่แล้ว

    Thanks sir

  • @jelleposthuma8786
    @jelleposthuma8786 4 ปีที่แล้ว

    Good explanation! Currently just started my first year of geology, so identifying these is still very hard for me. One question, is identifying based on vegetation accurate enough? How do you know the increase of minerals is caused by a fault and not by just regular sediment deposits?

    • @GEOCAMPInstitute_iso
      @GEOCAMPInstitute_iso 2 ปีที่แล้ว

      Really, it's all about integrating all data you can get. Vegetation is a good start, but the regional geology, structural history and other evidence of displacements need to be considered for more accurate interpretation. I hope this helps.

  • @ranujdas638
    @ranujdas638 4 ปีที่แล้ว

    Thank you sir

  • @Cooldipo
    @Cooldipo 4 ปีที่แล้ว

    Hey bros, i just want to know that you are doing a great job....the views will come with time, don't slow down please. I am impressed to hear someone like me do so much justice to this science. Much love

  • @sayantanghosh6714
    @sayantanghosh6714 4 ปีที่แล้ว

    Great

  • @kessdeameta4566
    @kessdeameta4566 4 ปีที่แล้ว

    This is great. I relished every second of it. Thanks @Dr Ifeanyi and @GEOCAMP Institute

    • @GEOCAMPInstitute_iso
      @GEOCAMPInstitute_iso 4 ปีที่แล้ว

      Glad it was worth your time. Pls help share link and subscribe

  • @salmamaaou3050
    @salmamaaou3050 4 ปีที่แล้ว

    thank you

  • @salmamaaou3050
    @salmamaaou3050 4 ปีที่แล้ว

    Thanks a lot for your great video

  • @sreekarthik4864
    @sreekarthik4864 4 ปีที่แล้ว

    Really Helpful. Elaborate explaination. THANKS!!

  • @ahmedkoko3940
    @ahmedkoko3940 4 ปีที่แล้ว

    Thanks my teacher you are doing great job for Africans

  • @thandekamlambo5171
    @thandekamlambo5171 4 ปีที่แล้ว

    This is really useful. How can you identify an MRS and TST within a fluvial/deltaic environment?

  • @thandekamlambo5171
    @thandekamlambo5171 4 ปีที่แล้ว

    I really wish you were my lecturer at university. Thank you for this

    • @GEOCAMPInstitute_iso
      @GEOCAMPInstitute_iso 4 ปีที่แล้ว

      Well, thanks for the compliment 🙂. Glad you liked it.

    • @thandekamlambo5171
      @thandekamlambo5171 4 ปีที่แล้ว

      GEOCAMP Institute is it possible to do a video on passive margins and sub-basins?

    • @GEOCAMPInstitute_iso
      @GEOCAMPInstitute_iso 4 ปีที่แล้ว

      Noted Thandeka.Hopefully one of our future videos will discuss it.

  • @ashutoshmishra4013
    @ashutoshmishra4013 4 ปีที่แล้ว

    Tq for uploading such lecture videos