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multiphysics finite element physical modeling program  (COMSOL Inc)
90
COMSOL Inc multiphysics finite element physical modeling program
( A , C , and E ) The geometries and boundary conditions of COMSOL <t>Multiphysics</t> finite element thermal models for schematic cross sections of the crust and upper mantle in the region of the CE5 landing site. Compositions and thermal conductivities used for all models are shown in (A) and discussed in Materials and Methods. The upper KREEP layer represents Imbrium ejecta to the east of the CE5 landing site and begins generating heat at 3.9 Ga in all models. The lower KREEP layer has the composition of high-K KREEP . See Materials and Methods for more details on initial model conditions. ( B , D , and F ) Model results showing the temperature profiles of the crust and upper mantle at 2 Ga for each model. As these models are purely conductive and absolute temperatures are not necessarily applicable to the mantle, but rather these models show the relative heating effects of a subcrustal KREEP layer of either 5 km (D) or 10 km (F) thickness.
Multiphysics Finite Element Physical Modeling Program, supplied by COMSOL Inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/result/multiphysics finite element physical modeling program/product/COMSOL Inc
Average 90 stars, based on 1 article reviews
multiphysics finite element physical modeling program - by Bioz Stars, 2026-04
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finite element solver program ansys 2022  (ANSYS inc)
90
ANSYS inc finite element solver program ansys 2022
( A , C , and E ) The geometries and boundary conditions of COMSOL <t>Multiphysics</t> finite element thermal models for schematic cross sections of the crust and upper mantle in the region of the CE5 landing site. Compositions and thermal conductivities used for all models are shown in (A) and discussed in Materials and Methods. The upper KREEP layer represents Imbrium ejecta to the east of the CE5 landing site and begins generating heat at 3.9 Ga in all models. The lower KREEP layer has the composition of high-K KREEP . See Materials and Methods for more details on initial model conditions. ( B , D , and F ) Model results showing the temperature profiles of the crust and upper mantle at 2 Ga for each model. As these models are purely conductive and absolute temperatures are not necessarily applicable to the mantle, but rather these models show the relative heating effects of a subcrustal KREEP layer of either 5 km (D) or 10 km (F) thickness.
Finite Element Solver Program Ansys 2022, supplied by ANSYS inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/result/finite element solver program ansys 2022/product/ANSYS inc
Average 90 stars, based on 1 article reviews
finite element solver program ansys 2022 - by Bioz Stars, 2026-04
90/100 stars
  Buy from Supplier
three-dimensional (3d) finite element model (fem) program  (Abaqus Inc)
90
Abaqus Inc three-dimensional (3d) finite element model (fem) program
( A , C , and E ) The geometries and boundary conditions of COMSOL <t>Multiphysics</t> finite element thermal models for schematic cross sections of the crust and upper mantle in the region of the CE5 landing site. Compositions and thermal conductivities used for all models are shown in (A) and discussed in Materials and Methods. The upper KREEP layer represents Imbrium ejecta to the east of the CE5 landing site and begins generating heat at 3.9 Ga in all models. The lower KREEP layer has the composition of high-K KREEP . See Materials and Methods for more details on initial model conditions. ( B , D , and F ) Model results showing the temperature profiles of the crust and upper mantle at 2 Ga for each model. As these models are purely conductive and absolute temperatures are not necessarily applicable to the mantle, but rather these models show the relative heating effects of a subcrustal KREEP layer of either 5 km (D) or 10 km (F) thickness.
Three Dimensional (3d) Finite Element Model (Fem) Program, supplied by Abaqus Inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/result/three-dimensional (3d) finite element model (fem) program/product/Abaqus Inc
Average 90 stars, based on 1 article reviews
three-dimensional (3d) finite element model (fem) program - by Bioz Stars, 2026-04
90/100 stars
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finite element method (fem)–ansys program  (ANSYS inc)
90
ANSYS inc finite element method (fem)–ansys program
( A , C , and E ) The geometries and boundary conditions of COMSOL <t>Multiphysics</t> finite element thermal models for schematic cross sections of the crust and upper mantle in the region of the CE5 landing site. Compositions and thermal conductivities used for all models are shown in (A) and discussed in Materials and Methods. The upper KREEP layer represents Imbrium ejecta to the east of the CE5 landing site and begins generating heat at 3.9 Ga in all models. The lower KREEP layer has the composition of high-K KREEP . See Materials and Methods for more details on initial model conditions. ( B , D , and F ) Model results showing the temperature profiles of the crust and upper mantle at 2 Ga for each model. As these models are purely conductive and absolute temperatures are not necessarily applicable to the mantle, but rather these models show the relative heating effects of a subcrustal KREEP layer of either 5 km (D) or 10 km (F) thickness.
Finite Element Method (Fem)–Ansys Program, supplied by ANSYS inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/result/finite element method (fem)–ansys program/product/ANSYS inc
Average 90 stars, based on 1 article reviews
finite element method (fem)–ansys program - by Bioz Stars, 2026-04
90/100 stars
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finite element software program ansys workbench 18.0  (ANSYS inc)
90
ANSYS inc finite element software program ansys workbench 18.0
( A , C , and E ) The geometries and boundary conditions of COMSOL <t>Multiphysics</t> finite element thermal models for schematic cross sections of the crust and upper mantle in the region of the CE5 landing site. Compositions and thermal conductivities used for all models are shown in (A) and discussed in Materials and Methods. The upper KREEP layer represents Imbrium ejecta to the east of the CE5 landing site and begins generating heat at 3.9 Ga in all models. The lower KREEP layer has the composition of high-K KREEP . See Materials and Methods for more details on initial model conditions. ( B , D , and F ) Model results showing the temperature profiles of the crust and upper mantle at 2 Ga for each model. As these models are purely conductive and absolute temperatures are not necessarily applicable to the mantle, but rather these models show the relative heating effects of a subcrustal KREEP layer of either 5 km (D) or 10 km (F) thickness.
Finite Element Software Program Ansys Workbench 18.0, supplied by ANSYS inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/result/finite element software program ansys workbench 18.0/product/ANSYS inc
Average 90 stars, based on 1 article reviews
finite element software program ansys workbench 18.0 - by Bioz Stars, 2026-04
90/100 stars
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finite element program comsol multiphysics  (COMSOL Inc)
90
COMSOL Inc finite element program comsol multiphysics
( A , C , and E ) The geometries and boundary conditions of COMSOL <t>Multiphysics</t> finite element thermal models for schematic cross sections of the crust and upper mantle in the region of the CE5 landing site. Compositions and thermal conductivities used for all models are shown in (A) and discussed in Materials and Methods. The upper KREEP layer represents Imbrium ejecta to the east of the CE5 landing site and begins generating heat at 3.9 Ga in all models. The lower KREEP layer has the composition of high-K KREEP . See Materials and Methods for more details on initial model conditions. ( B , D , and F ) Model results showing the temperature profiles of the crust and upper mantle at 2 Ga for each model. As these models are purely conductive and absolute temperatures are not necessarily applicable to the mantle, but rather these models show the relative heating effects of a subcrustal KREEP layer of either 5 km (D) or 10 km (F) thickness.
Finite Element Program Comsol Multiphysics, supplied by COMSOL Inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/result/finite element program comsol multiphysics/product/COMSOL Inc
Average 90 stars, based on 1 article reviews
finite element program comsol multiphysics - by Bioz Stars, 2026-04
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finite element code ansys; finite element program (fea), release 14, sas ic  (ANSYS inc)
90
ANSYS inc finite element code ansys; finite element program (fea), release 14, sas ic
( A , C , and E ) The geometries and boundary conditions of COMSOL <t>Multiphysics</t> finite element thermal models for schematic cross sections of the crust and upper mantle in the region of the CE5 landing site. Compositions and thermal conductivities used for all models are shown in (A) and discussed in Materials and Methods. The upper KREEP layer represents Imbrium ejecta to the east of the CE5 landing site and begins generating heat at 3.9 Ga in all models. The lower KREEP layer has the composition of high-K KREEP . See Materials and Methods for more details on initial model conditions. ( B , D , and F ) Model results showing the temperature profiles of the crust and upper mantle at 2 Ga for each model. As these models are purely conductive and absolute temperatures are not necessarily applicable to the mantle, but rather these models show the relative heating effects of a subcrustal KREEP layer of either 5 km (D) or 10 km (F) thickness.
Finite Element Code Ansys; Finite Element Program (Fea), Release 14, Sas Ic, supplied by ANSYS inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/result/finite element code ansys; finite element program (fea), release 14, sas ic/product/ANSYS inc
Average 90 stars, based on 1 article reviews
finite element code ansys; finite element program (fea), release 14, sas ic - by Bioz Stars, 2026-04
90/100 stars
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finite element method ansys mesh program  (ANSYS inc)
90
ANSYS inc finite element method ansys mesh program
( A , C , and E ) The geometries and boundary conditions of COMSOL <t>Multiphysics</t> finite element thermal models for schematic cross sections of the crust and upper mantle in the region of the CE5 landing site. Compositions and thermal conductivities used for all models are shown in (A) and discussed in Materials and Methods. The upper KREEP layer represents Imbrium ejecta to the east of the CE5 landing site and begins generating heat at 3.9 Ga in all models. The lower KREEP layer has the composition of high-K KREEP . See Materials and Methods for more details on initial model conditions. ( B , D , and F ) Model results showing the temperature profiles of the crust and upper mantle at 2 Ga for each model. As these models are purely conductive and absolute temperatures are not necessarily applicable to the mantle, but rather these models show the relative heating effects of a subcrustal KREEP layer of either 5 km (D) or 10 km (F) thickness.
Finite Element Method Ansys Mesh Program, supplied by ANSYS inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/result/finite element method ansys mesh program/product/ANSYS inc
Average 90 stars, based on 1 article reviews
finite element method ansys mesh program - by Bioz Stars, 2026-04
90/100 stars
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finite element software program ansys 2023 r2  (ANSYS inc)
90
ANSYS inc finite element software program ansys 2023 r2
( A , C , and E ) The geometries and boundary conditions of COMSOL <t>Multiphysics</t> finite element thermal models for schematic cross sections of the crust and upper mantle in the region of the CE5 landing site. Compositions and thermal conductivities used for all models are shown in (A) and discussed in Materials and Methods. The upper KREEP layer represents Imbrium ejecta to the east of the CE5 landing site and begins generating heat at 3.9 Ga in all models. The lower KREEP layer has the composition of high-K KREEP . See Materials and Methods for more details on initial model conditions. ( B , D , and F ) Model results showing the temperature profiles of the crust and upper mantle at 2 Ga for each model. As these models are purely conductive and absolute temperatures are not necessarily applicable to the mantle, but rather these models show the relative heating effects of a subcrustal KREEP layer of either 5 km (D) or 10 km (F) thickness.
Finite Element Software Program Ansys 2023 R2, supplied by ANSYS inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/result/finite element software program ansys 2023 r2/product/ANSYS inc
Average 90 stars, based on 1 article reviews
finite element software program ansys 2023 r2 - by Bioz Stars, 2026-04
90/100 stars
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( A , C , and E ) The geometries and boundary conditions of COMSOL Multiphysics finite element thermal models for schematic cross sections of the crust and upper mantle in the region of the CE5 landing site. Compositions and thermal conductivities used for all models are shown in (A) and discussed in Materials and Methods. The upper KREEP layer represents Imbrium ejecta to the east of the CE5 landing site and begins generating heat at 3.9 Ga in all models. The lower KREEP layer has the composition of high-K KREEP . See Materials and Methods for more details on initial model conditions. ( B , D , and F ) Model results showing the temperature profiles of the crust and upper mantle at 2 Ga for each model. As these models are purely conductive and absolute temperatures are not necessarily applicable to the mantle, but rather these models show the relative heating effects of a subcrustal KREEP layer of either 5 km (D) or 10 km (F) thickness.

Journal: Science Advances

Article Title: A shallow mantle source for the Chang’e 5 lavas reveals how top-down heating prolonged lunar magmatism

doi: 10.1126/sciadv.adr1486

Figure Lengend Snippet: ( A , C , and E ) The geometries and boundary conditions of COMSOL Multiphysics finite element thermal models for schematic cross sections of the crust and upper mantle in the region of the CE5 landing site. Compositions and thermal conductivities used for all models are shown in (A) and discussed in Materials and Methods. The upper KREEP layer represents Imbrium ejecta to the east of the CE5 landing site and begins generating heat at 3.9 Ga in all models. The lower KREEP layer has the composition of high-K KREEP . See Materials and Methods for more details on initial model conditions. ( B , D , and F ) Model results showing the temperature profiles of the crust and upper mantle at 2 Ga for each model. As these models are purely conductive and absolute temperatures are not necessarily applicable to the mantle, but rather these models show the relative heating effects of a subcrustal KREEP layer of either 5 km (D) or 10 km (F) thickness.

Article Snippet: A series of two-dimensional thermal evolution models for a simplified east-west cross section of the local region of the Moon in northern Oceanus Procellarum where the CE5 basalts were collected were constructed using the COMSOL Multiphysics finite element physical modeling program.

Techniques: