top of page
Logo.png

What is DDT?

DDT & Conventional Exploration

The DDT Survey Process

DDT vs. Indirect Methodologies

What is ddt?

A proprietary geophysical methodology

DDT™ is a proprietary geophysical methodology developed to detect and delineate subsurface hydrocarbon accumulations.


The technology is based on OGD's interpretation of naturally and occurring intrinsic radiation associated with matter in the Earth's crust. DDT converts latent mineral-correlated signatures recorded in the silver-halide emulsion of analog satellite imagery into detectable and spatially recovered evidence of target mineralization. According to the DDT™ scientific model, physical materials in an excited state — driven by the influence of Earth's geophysical fields — generate distinctive energy signatures associated with Super Small Subatomic Particles (3SP) and their corresponding radiation phenomena.

OGD's laboratory and field systems are designed to analyze the measurable effects associated with these phenomena—including characteristic reflections, shadows, tracks, frequencies, amplitudes, and phase relationships.


Different elements and compounds are interpreted as producing distinctive intrinsic radiation spectra. These signatures form cluster and macro-cluster field structures that can be analyzed to identify variations within subsurface formations and evaluate the possible presence and distribution of hydrocarbons.

Direct Detection Technology: the example of hydrocarbon exploration

Direct Detection Technology (DDT) is a proprietary geophysical methodology developed to detect and delineate subsurface hydrocarbon and mineral accumulations — based on OGD's interpretation of naturally occurring intrinsic radiation associated with matter in the Earth's crust

Image (Grand Canyon aerial view — exposed geological strata representing the exploration e
Image5.png

The video shows passive satellite imaging of the surface being conducted

Richard Feynman QED and DDT

The video shows passive satellite imaging of the surface being conducted

Read Article

ddt & conventional exploration

How DDT™ complements conventional exploration

Traditional hydrocarbon exploration commonly involves a sequence of geological, geochemical, geophysical, and drilling activities, including:

map.png

Geological mapping and regional evaluation

satellite (1).png

Field reconnaissance, aerial photography, and satellite analysis

flask-conical.png

Geochemical sampling of soils, sediments, and other materials

activity.png

Gravity, magnetic, resistivity, and 2D/3D seismic surveys

drill.png

Exploratory drilling, well logging, testing, and reservoir evaluation

These methods remain important components of petroleum exploration, but they can require significant capital, extensive field operations, and long project timelines.

DDT™ is designed to complement and potentially reduce the scope of conventional exploration by identifying and prioritizing prospective areas before companies commit to more expensive seismic programs or exploratory drilling.

The DDT™ Survey Process

Satellite reconnaissance, imagery collected, then airborne field survey

Each stage narrows the search area — from a broad territory to a small, graded target zone

Reconnaissance study

Star One

397aabe6da8758459ec53a9c4026d2cf4ac4794c.png

Prospective district · Yellow contour

The first stage uses OGD's proprietary Star One, Star Two and Stage One Surveys to evaluate large geographic areas from satellite data. Star One is designed as a large-area reconnaissance program, typically covering approximately 5,000–100,000 km² and more, depending on the geological setting, exploration objectives, accessibility, and operational environment. Its primary objective is to establish whether geophysical signatures consistent with the targeted mineralization are present within the surveyed territory or offshore area.

​

The process includes:

  • Analysis of satellite imagery using proprietary processing techniques

  • Identification of anomalous signatures associated with target resources

  • Preliminary evaluation of the presence or absence of prospective hydrocarbon zones

  • Definition of the general geographic boundaries of identified anomalies

  • Selection and prioritization of areas for detailed Stage Two investigation

​

A reconnaissance area of approximately 100 km × 100 km can typically be evaluated within approximately 4-5 weeks, depending on project requirements and data availability.

Enlarged study of the prospective district

Star Two

d3a5d3fa23e2c3d4e0f91b5f23edc2df19abf153.png

Prospective area · Green contour

Star Two focuses on the prospective areas identified during Star One. Enlarged primary anomalies associated with the target mineral’s own radiation are recorded and ranked by significance. Based on the distribution and relative strength of these anomalies, enlarged prospective areas are delineated, providing a more precise basis for geological interpretation and subsequent target grading and exploration.

Detailed study of the enlarged prospective area

Stage One

0dbd7a36bdf0e940fddc3057beb6396dda610ca3.png

Prospective area · Blue contour

Stage One focuses on identifying primary anomalies associated with the target mineral’s own radiation. The detected anomalies are recorded and ranked by significance, allowing prospective areas to be delineated for further analysis and more detailed investigation in subsequent survey stages.

Airborne Field Survey

Stage Two

88e82e00f1d4da2b1e2c10e96abff951ab570ab7.png

Prospective area · Blue contour

Priority areas identified during satellite reconnaissance can be investigated using helicopter or low-altitude aircraft equipped with OGD's GEO-SCAN ML3 and MLS-3 survey system. The system incorporates specialized mono-spectrometers calibrated for selected elements and compounds. There are two models of DDT field equipment: for airborne survey and compact back pack model. DDT field equipment set is portable and may be installed on ATW, helicopter, low speed boats or planes. Compact model may be packed as a backpack and carried by person.

​

Stage Two surveys are designed to generate high-resolution digital interpretations showing:

​

  • Intrinsic radiation intensity

  • Geographic extent of interpreted hydrocarbon accumulations

  • Prospective drilling locations

  • Estimated depth and thickness relationships

  • Spatial distribution of targeted subsurface formations

​

Survey results can be presented as color-coded maps, topographic overlays, cross-sections, and 3D block diagrams to support geological interpretation and drilling decisions.

Direct detection vs. indirect methodologies

DDT vs. today's exploration technologies

DDT is different because it is designed to detect the resource signature itself — not only the surrounding geological clues

Technology
What It Mainly Detects
Key Limitation
DDT Advantage
Magnetics and Gravity
Physical-property contrasts
Shows structures and anomalies, not certainty of mineral type
DDT focuses on target identification
Satellite / hyperspectral
Surface mineral indicators
Mostly surface or alteration mapping
DDT aims beyond surface indicators
Geochemistry / Сore / CC
Physical samples and lab analysis
Slow, local, expensive, late-stage
DDT can screen large areas faster
Electromagnetic Surveys
Conductivity and resistivity contrasts
Strong for conductive bodies, weaker for non-conductive targets; sensitive to noise, metal objects and soil conditions
DDT is less sensitive to EM interference
AI Prediction (KoBold)
AI prediction from existing geological data
Depends on data quality and model assumptions
DDT generates direct detection intelligence
Muon Tomography (Ideon)
Subsurface density using muon tomography
Requires local deployment; detects density anomalies, not resource identity
DDT targets resource-specific signatures
bottom of page